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5ª CO
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5TH PORT
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ALGARVE
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a. The
e. We
ery in
anned
In IV
M
Phot
snow
of m
studi
(tem
expe
melte
consi
that
Reso
radia
was
const
also a
were
~20 t
snow
const
and t
DOM
calcu
phot
phot
ERCURY PH
Man
2 Me
ochemical r
w. The balan
mercury rem
ies in snow
perature, ir
eriments tha
ed snow u
isted of a Lu
can hold 1
olute Bay, N
ation intensi
quantified.
tants of mer
analysed for
e analysed fo
to 600 pg, a
w total phot
tants range
the rate con
M, and the ch
ulate both th
oreduction
ochemical lo
HOTOCHEMI
nn, E.1, Mal
1 Acad
morial Univer3 Envir
reduction an
nce between
aining in sn
w primarily
rradiation i
at facilitate
under contr
uzchem pho
– 10 ultra
U, in March
ties (1.26 ‐ 5
Total phot
rcury in snow
r DOM, fluo
or total merc
and the rate
toreducible
d between
nstant for m
hloride conc
he amount
in snow.
oss in snow
CAL OXIDA
M
lory, M.1, Zi
dia University
rsity of Newf
onment Cana
nelson.o
nd volatiliza
n photochem
now at the
have bee
ntensity) a
the study o
rolled envir
toreactor pl
violet (UV)
h 2012, was
5.78 Wm‐2 fo
oreduced m
w were dete
rescence an
cury. In froz
constants f
mercury am
~0.03 – 0.3
ercury redu
centration in
of photored
These equ
without the
ATION AND
MELTED SNO
iegler, S.2, T
y, Wolfville, N
foundland, St
ada, Halifax, N
odriscoll@ac
ation is the
mical oxidat
onset of m
n field stu
are variable
of mercury
ronmental
laced in a w
) bulbs. Fro
subjected
or 280 to 4
mercury and
ermined usin
nd ion conce
en snow, to
for mercury
mounts were
30 h‐1. Both
uction in the
n the snow.
ducible mer
uations wil
e need for ex
REDUCTION
OW
Tordon, R.3
ova Scotia, C
Johns, Newf
Nova Scotia, C
cadiau.ca
primary los
ion and red
melt. To dat
udies where
. This rese
photochem
conditions.
alk‐in fridge
ozen and m
to several e
00 nm), and
d the pseud
ng curve fitt
entrations. N
otal photored
reduction w
e ~10 – 3500
the amount
e samples we
Empirical r
rcury and th
ll aid in t
xtensive field
N IN ARCTIC
3, O’Driscoll
anada
oundland, Ca
Canada
s mechanism
uction regu
te, mercury
e environm
earch devel
mical reactio
The expe
(4 °C) or fre
melted snow
environment
d the photo
do‐first orde
ting. Irradiat
Non‐irradiate
ducible merc
were ~0.1 to
0 pg, and th
t of photore
ere related t
elationships
he rate cons
the predict
d sampling.
Págin
C FROZEN A
l, N.1
anada
m for merc
lates the am
y photochem
mental cond
loped labor
ns in frozen
erimental sy
eezer (‐10 °C
w, collected
tally relevan
o‐produced
er reduction
ted samples
ed snow sam
rcury ranged
0.5 h‐1. In m
he reduction
educible me
to UV irradi
s were deriv
stant for me
tion of me
a | 25
AND
ury in
mount
mistry
ditions
ratory
n and
ystem
), and
from
nt UV
Hg(0)
n rate
were
mples
d from
melted
n rate
ercury
ation,
ved to
ercury
ercury
ARS
CQ
Fildes
one o
Cu, C
Great
Eleph
collec
In wa
lowe
conc
Comp
with
levels
conc
conc
conta
The o
betw
gove
The h
wate
prom
lowe
ENIC, CU, C
SOILS
Eduard
QE, Instituto S
s Peninsula
of the most
Cd, Zn, Pb an
t Wall Bay (
hant Bay (CN
cted near Ru
ater samples
st values r
entrations o
pared to wa
all studied
s varied bet
entrations
entrations o
aminated so
organic matt
ween LOI an
erned by ant
high levels o
er may be e
moted their
r availability
CD, HG, ZN
S OF FILDES
o Amaro, A
Superior Técn
is located in
polluted pla
nd Hg), sedi
GM1‐GM6),
N1‐CN4), Ard
ussian statio
s (fresh and
reported in
of Cu up to 9
ater samples
trace eleme
tween 140 μ
were belo
obtained for
oil” accordin
ter content
nd trace ele
hropogenic
of contamina
explained b
absorption
y of contami
AND PB CO
S PENINSUL
André Mão
nico, Universit
eduardo.la
n King Georg
aces in Antar
ments and w
a small river
dley Island (A
on (SVB1‐SVB
d saline) trac
other loca
90 times high
s, sediments
ents presen
μg.g‐1 (CN1)
ow 0.35 μg
r Pb and also
g to the Por
(%LOI) varie
ement leve
deposition r
ants in sedim
by the relat
by particles
nants to the
ONTAMINAT
LA, KING GE
de Ferro, A
ty of Lisbon, A
anceiro.amaro
ge Island, on
rctica. In ord
water samp
r between t
AA1‐AB3) an
B5) and near
ce element c
ations in An
her were fou
s and soils s
nting much h
and 19 000
g.L‐1. It is
o for Cu in T
rtuguese and
ed between
ls. This sug
rather than
ments and s
tively high
s. In turn, th
e aquatic org
TION IN THE
EORGE ISLA
Ana Maria M
Av. Rovisco P
ne of the So
der to track
ples were co
the Chilean a
nd Collins Ba
r the fuel tan
concentratio
ntarctica. A
und (0.85 μg
showed a co
higher conc
0 μg.g‐1 (T1)
worthwhil
T1 correspon
d European
0.8 and 8% a
ggests that
by natural in
soils and the
LOI conten
he high LOI
ganisms.
E WATER, S
ND, ANTAR
Mota, João
Pais, 1049‐001
uth Shetlan
inputs of tra
llected at Fi
and Russian
y (C1‐C4). So
nks (T1‐T4).
ons were co
Although at
g.L‐1).
ompletely d
centrations.
while in w
e to emph
nd to a class
laws.
and no corre
contaminan
nputs.
e correspond
t in the so
content ma
Págin
SEDIMENTS
RCTICA
Canário
Lisboa Portu
d Islands, an
ace element
ildes Bay (F1
n Stations (R
oils samples
onsistent wit
Great Wal
ifferent sce
For examp
water sample
hasize that
sification of
elation was f
nt distribut
dent low lev
olid fraction
y contribute
a | 26
AND
ugal
nd it’s
ts (As,
1‐F13),
R1‐R2),
were
th the
ll Bay
nario,
le, Pb
es, Pb
t the
“high
found
ion is
vels in
n that
e to a
1 Lab
Since
conc
data,
summ
The a
the G
(GPS
desig
on a
This v
influe
partic
remo
latitu
the s
proce
Signif
a thre
2006
no re
defor
DEC
G
boratorio de
e the establi
ern was add
, surface def
mer campaig
automated d
Global Navig
), are valued
gn of a wirel
control cent
volcano Ant
ences to the
cularly dem
otely superv
ude no GPS
south directi
essing strate
ficant groun
ee years ext
6‐2007 camp
eported incr
rmation also
CEPTION ISL
Gonçalo Pra
Astronomía, 2 Centro d
3 Instituto S
ishment of t
dressed to t
formation d
gns, to provi
data acquisi
gation Satell
d features in
less connect
ter. Also, on
tarctic locati
e measured g
anding on b
ise the equip
satellite cro
ion due to t
egy to achie
nd deformat
tension proc
aign had on
ease of gas
o result from
LAND’S VOL
ates1,2,3, Ma
Geodesia y C
de Estudos Ge
Superior de E
gp
the Spanish
his island vo
ata has beco
ide forewarn
tion and pro
ite Systems
n surface def
tion infrastr
e site therm
on provide a
geophysical
both sensor
pment assur
osses the m
their orbital
ve the mand
tion was ide
cess present
ne of the low
emissions, i
m its tectonic
LCANO DEF
anuel Berro
Cartografía – F
eográficos – U
Engenharia –
prates@ualg
Base Gabrie
olcano’s dyn
ome availab
ning to thos
ocessing, an
(GNSS), in
formation su
ructure that
mometric dat
an environm
data. Also t
rs and comm
res their ma
eridian from
planes 55º e
datory millim
entified in th
t throughout
west number
n contrast w
c surroundin
ORMATION
coso1 and L
Facultad de C
Universidade
Universidade
.pt
el de Castilla
namics. In ad
le in near re
se that visit o
nd the posit
particular th
urveillance.
allows data
ta at various
ment practic
this remote
munications.
ximum retu
m zenith to
equatorial in
meter level p
he 2003‐2004
t the 2006‐2
r of detecte
with 2003‐20
ngs, where it
SURVEILLA
LAGC Group
iencias – Univ
de Lisboa
do Algarve
a in Decepti
ddition to th
eal‐time alon
or research t
ioning preci
he Global Po
The data ac
a processing
s depths is a
ally free fro
and inhospit
. The additio
rn. Moreove
low angles
nclination, re
precisions.
4 austral sum
2007 campai
d seismic ev
004. Decepti
t acts as a st
Págin
ANCE
p1
versidad de C
on Island, s
he seismic ac
ng this last a
there.
ision and rat
ositioning Sy
ccess require
g in near rea
ccessed.
m anthropo
table contin
onal capabil
er, at Decep
above horiz
requiring an
mmer just b
ign. Howeve
vents per da
ion Island gr
train marker
a | 27
Cádiz
pecial
ctivity
ustral
tes of
ystem
ed the
l‐time
ogenic
nent is
lity to
ption’s
zon in
extra
before
er, the
ay and
round
r.
PR
Mar
The w
const
warm
slight
aims
bette
With
evolu
Byers
const
Durin
we co
follow
Geoc
these
recor
from
RELIMINARY
(LIVING
rc Oliva1, De
1 Insti2 Fac
3
4 Parqu5 Centro
western par
titutes an a
ming recorde
t decrease
to provide
er frame this
this purpo
ution in Bye
s Peninsula
titutes the la
ng the first f
ollected the
wing the deg
chemical, bio
e cores. In t
rds. Accordi
the Early an
Y RESULTS O
GSTON ISLA
ermot Anto
tute of Geog
cultad de Cien Institute of E
ue Natural De
de Estudios y6 Centre d'
rt of the Ant
area with s
ed during th
in the rate
accurate da
s warming tr
ose, we foc
rs Peninsula
is the weste
argest ice‐fr
field work c
e complete s
glaciation of
ological and
this commun
ng to these
nd Mid‐Holo
ON THE HO
AND, ANTAR
oniades2, S.
Pla‐Rabe
raphy and Sp
ncias, Univers
Earth Sciences
Peñalara, Ce
y Experiment
'Estudis Avan
oliva_
tarctic Penin
significant i
he second h
of warming
ta on the Ho
rend within
cused on th
a using lake
ernmost par
ee area in th
ampaign of
sedimentary
f Byers: Che
d geochrono
nication we
preliminary
cene.
OLOCENE D
RCTICA) INF
. Giralt3, Ign
es6 & Gonça
patial Planning
sidad de la Re
s Jaume Alme
entro de Inves
tación de Obr
nçats de Blane
_marc@yaho
nsula, where
inter‐annual
half of the X
g during the
olocene clim
the natural
he reconstru
sediments
rt of Livings
his archipela
the HOLOA
y sequence o
ster, Escond
ological stud
introduce t
y data, the d
EGLACIATIO
FERRED FRO
nacio Grana
alo Vieira1
g, University
epública, Mon
era (CSIC), Ba
stigación y Ge
ras Publicas (C
es (CEAB), Bla
o.com
e the South
l climate va
XXI century h
e last decad
mate conditi
climate varia
uction of t
as the basis
ston Island (
ago.
ANTAR proje
of four lakes
dido, Cerro N
dies are bein
the first AM
deglaciation
ON OF BYER
OM LAKE RE
ados4, Manu
of Lisbon, Po
ntevideo, Uru
arcelona, Spa
estión, Madrid
CEDEX), Madr
anes, Spain
Shetland Isl
ariability. H
has been of
de. The HOL
ons in this r
ability in the
he Holocen
s to infer cli
(South Shet
ect (Novemb
s distributed
Negro and D
ng undertak
MS C14 datin
process in
Págin
RS PENINSU
ECORDS
uel Toro5, S
ortugal
uguay
in
d, Spain
rid, Spain
ands are loc
ere, the cl
~2.5ºC, des
LOANTAR p
region in ord
e region.
ne environm
imate condi
tland Islands
ber‐Decemb
d along a tra
Domo lakes.
ken on seve
ngs for these
Byers dates
a | 28
ULA
Sergi
cated,
imate
pite a
roject
der to
mental
itions.
s) and
ber’12)
ansect
eral of
e lake
s back
C
1 Cen
2 So
3 De4 Divis
6 D
7 Dep
Multi
terre
our k
linkag
morp
Moun
cyano
sheet
to t
comm
youn
salts
conc
simp
organ
levels
funda
Anta
AT LIMITS
CONST
atarina Ma
ntre of Marine
outh Australia
epartment of B
sion of Mathe
5 Gateway An
Department of
partment of O8 College of
itrophic co
estrial ecosy
knowledge a
ge between
phology and
ntains, 80◦S
obacteria, li
ts, and soil
he diversit
munities, in
ger drifts (H
content (t
entration fr
le communi
nisms analy
s of biotic
amental to
rctic soil eco
OF LIFE: M
TRAINTS ON
galhães1, M
Storey5, D
e and Environ
an Museum, G
Scienc
Biological Scie
ematical and N
tarctica, Univ
f Biology and
Organismic Bio
Earth, Ocean
mmunities
stems, whil
about the lim
n the divers
d soil geoc
S). We ex
ichens, alga
physicochem
y of the
terms of t
Hatherton a
thus lower
rom younger
ties, in term
ysed. This s
communitie
understand
osystems.
MULTIDISCIP
N BIOTIC D
Mark I Steve
Diana Wall6,
mental Resea
4050‐
GPO Box 234, A
ces, University
ences, Univers
Natural Scienc
A
versity of Cant
Natural Resou
Collin
ology, Univers
and Environm
cmaga
that maint
e the simpl
mits to life o
sity of diffe
chemistry in
amined the
e, invertebr
mistry. Resu
organisms
trophic leve
nd Britannia
conductivit
r to older dr
ms of numbe
study revea
es with abio
environmen
PLINARY INS
IVERSITY IN
ens2, Steph
, Roman Tü
arch, Universit
‐123 Porto, Po
Adelaide SA 50
y of Adelaide,
sity of Waikat
ces, Arizona St
AZ 85306, USA
terbury, Priva
urce Ecology L
ns, CO 80523,
sity of Salzbur
ment, Universi
alhaes@ciima
tain the fu
est of any
on earth. In t
erent troph
n the remo
e distributi
rates) with r
ults showed
across diff
l diversity,
a) with high
ty). Our res
rift regions
r of trophic
led that int
otic spatial
ntal constra
SIGHTS REV
N CONTINEN
en C Cary3,8
ürk7, Ulrike
ty of Porto, Po
ortugal
000, and Scho
, SA 5005, Aus
to, Private Bag
tate Universit
A.
te Bag 4800,
Laboratory, C
USA.
rg, Hellbrunne
ity of Delawar
ar.up.pt
unctionality
natural com
this study, w
ic level com
ote Transan
on and di
respect to e
an abiotic s
ferent trop
were relate
her soil C/N
sults indica
drives a suc
levels and d
tegrating d
heterogene
ints influenc
VEAL ENVIRO
NTAL ANTAR
8, Becky A B
Ruprecht7
ortugal, Rua d
ool of Earth an
stralia.
g 3105, Hamilt
ty at the West
Christchurch,
olorado State
erstr. 34, 5020
re, Lewes, Del
of the ex
mmunity, are
we describe
mmunities t
ntarctic Mo
versity of
elevation, ag
spatial grad
phic levels.
ed to the w
ratio and low
te that an
ccession of c
diversity with
iversity acro
ity and geo
cing biologic
Págin
ONMENTAL
RCTICA
Ball4, Bryan
dos Bragas, nº
nd Environme
ton, New Zeal
t Campus, Gle
New Zealand
e University, F
0 Salzburg, Au
laware, USA.
xtreme Ant
e still challe
and interpre
to the geolo
ountains (D
biota (bac
ge of glacia
ient with re
More com
weakly deve
wer total so
increase o
complex to
hin each gro
oss multi‐tr
ological hist
cal distribut
a | 29
L
n C
289,
ental
land.
ndale,
d.
Fort
ustria.
tarctic
nging
et the
ogical
arwin
cteria,
l drift
espect
mplex
loped
oluble
of ion
more
oup of
rophic
ory is
tion in
EFF
José
M
1 In
4
Curre
majo
marin
for A
clima
chan
revie
clima
zoop
from
comp
provi
Anta
conse
FECTS OF E
é C. Xavier
M. Guerreiro
nstitute of M2 B
3 Universit
Centre of Fu
ent and new
or threats to
ne areas are
Antarctic sci
ate change.
ge in the st
w current a
ate change a
plankton, An
Antarctica
prehensive s
ide modellin
rctic specie
ervation, po
ENVIRONME
1,2, S. Loure
o1, A. R. Gon
Cruz1, V
arine Researc
British Antarct
ty of Lisbon,
nctional Ecol5 University
w projected
o the structu
e warming f
ience is to
While addr
tructure and
and expecte
and how it m
ntarctic krill,
a and the
species‐spec
ng analyses
es. Priorities
olicy making,
ENTAL CHAN
SOU
enço3, F. R.
nçalves1, S.
V. Paiva1, J.
ch (IMAR‐CM
tic Survey, Hig
Faculty of Sci
ogy, Departm
y of Algarve, F
JC
climate ch
ure and func
faster than a
develop mo
ressing the
d functionin
d overall fu
might affect v
fish, cephal
Southern
cific vulnera
s on the po
s for future
, education a
NGE IN THE
UTHERN OC
Ceia1, S. Ta
Pedro4, T. V
A. Ramos1
MA), University
gh Cross Mad
iences, Camp
ment of Life S
FCMA, Gambe
anges are u
ctioning of m
anywhere o
odels for as
question “W
ng of the A
ture change
various orga
lopods, mar
Ocean are
bility assess
otential hab
e research
and outreac
STRUCTUR
CEAN
vares4, L. K
Valente1, N
and J. C. M
y of Coimbra,
dingley Road,
po Grande, 174
Sciences, Univ
elas, 8000 Fa
net
unpreceden
marine ecos
on Earth. On
ssessing cur
What are th
Antarctic ma
es in the Sou
anisms in th
rine mamma
e sufficient
sments poss
bitat and di
work, alon
ch will be dis
E AND FUN
Kruger1, J. S
. Velez5, P.
arques1
, 3001‐401 Coi
, Cambridge,
49‐016 Lisbon
versity of Coim
ro, Portugal
ted in magn
ystems wor
e of the gre
rrent and fu
he effects o
rine ecosyst
uthern Ocea
is polar regio
als and seab
tly well st
sible. Theref
istribution o
ng with its
scussed.
Págin
NCTION OF T
Seco1, P. Alv
Azinhaga1,
imbra, Portug
UK
n, Portugal
mbra, Portug
nitude, and
rldwide. Ant
eatest challe
uture impac
of environm
tem?” we b
an in respon
on. These in
birds. Few sp
tudied to
fore, we wi
of poorly k
implication
a | 30
THE
vito1,
B.
gal
gal
pose
tarctic
enges
cts of
mental
briefly
nse to
nclude
pecies
make
ll also
nown
ns on
MER
Sílv
Wand
beca
of ad
the
conc
verte
expla
plasm
samp
blood
the f
older
years
feath
highe
1). D
differ
high
sugg
much
body
sex o
suffic
RCURY LEVE
via Tavares1
4
dering albat
use of popu
dult and juve
food chain
entrations
ebrate, incl
anations for
ma and bloo
pled at Bird
d componen
eathers of y
r pre‐breede
s, 20.14±7.64
hers of pre‐
er in blood c
Differences i
rences in tro
feather me
ests either a
h more likely
y mercury po
on mercury
cient to lowe
ELS IN THE
O
, José Xavie
1 Centre2 Institu
Centre for En
trosses (Diom
ulation declin
enile mortali
n and accu
in tissues o
uding close
r this patte
od cells of w
Island, Sou
nts of chick
young pre‐br
ers (aged 9‐
4 mg kg‐1).
‐breeders o
cells of bree
in mercury
ophic ecolog
ercury conce
a switch in d
y, an increas
ool becomes
levels in b
er the body
WANDERIN
F SEX, AGE
er2,3, Richar
e for Function
ute of Marine3 British Ant
nvironmental
stava
medea exula
nes since the
ity in longlin
umulates in
of the wan
ely related
ern, we me
wandering a
uth Georgia.
s (6.14±1.91
reeders (age
‐15 years, 21
There was
r breeding
eding female
levels betw
gy during th
entrations o
diet or distri
se in moult f
s reduced by
lood sugge
pool of mer
NG ALBATRO
E AND BREE
rd Phillips3,
nal Ecology, U
e Research, U
tarctic Survey
and Marine S
res@student
ans) are clas
e 1960s or 19
ne fisheries.
n top pred
ndering alb
species.
easured tota
albatrosses
Mercury co
and 0.84±0
ed 4‐6 years
1.20±6.32 m
no effect o
adults, whe
es (12.04±4.5
ween the se
e breeding r
of young p
ibution (and
frequency a
y its excretio
sts that ex
rcury in bree
OSS DIOME
EDING STAT
Maria E. Pe
University of C
University of C
y, Cambridge
Studies, Unive
t.uc.pt
ssified as Vu
970s, resulti
Although m
dators such
atross are
In order t
al mercury
of known a
oncentration
0.36 mg kg‐1
s, 48.13±6.34
g kg‐1) and
of sex on me
ereas mercu
55 mg kg‐1)
exes seem
rather than
re‐breeders
d hence expo
s birds appr
on into feath
cretion of m
eding female
DEA EXULAN
TUS
ereira4 and
Coimbra
Coimbra
ersity of Avei
lnerable in t
ing from uns
mercury bio‐a
h as albat
greater tha
to explore
concentrat
ge, sex and
ns were low
1 respective
4 mg kg‐1) th
breeding a
ercury conc
ury levels w
than males
therefore t
the nonbree
compared
osure to me
roach matur
hers. The sig
mercury into
es to below t
Págin
NS – INFLUE
Miguel Par
iro
the IUCN Re
sustainable
amplifies thr
trosses, me
an in any
the altern
ions in fea
d breeding s
w in feather
ly), and hig
han in feath
adults (aged
centrations i
were signific
(7.10±2.10 m
to largely r
eding period
with older
ercury in pre
rity, such tha
gnificant eff
o the egg i
that of male
a | 31
ENCE
rdal1
ed List
levels
rough
ercury
other
native
thers,
status
rs and
her in
ers of
d 11‐33
in the
cantly
mg kg‐
reflect
d. The
birds
ey) or,
at the
ect of
is not
es.
ASS
1 CEN
A 168
enha
and s
at th
treat
atten
bene
168 t
natur
“self
biost
reme
appli
incine
SESSMENT O
SOIL
Nazaré Cou
NSE, Departam
2 Departme3 Arctic Resea
8 days‐perio
nce soil rem
synergistic e
e end of the
tments, enh
nuation. The
efits of both
there was a
ral attenua
purification”
timulation w
ediation sche
ed through
eration facil
OF BIOREM
USING SUR
uto1*, Janne
mento de Ciê
Univ
ent of Civil En
arch Centre,
od field stud
mediation w
effects of bio
e first 42 da
hanced pet
e coupling of
h techniques
an opposite
ation which
” capacity
with active h
eme can be
out the yea
ity.
MEDIATION S
RPLUS HEAT
e Fritt‐Rasm
Alexa
ências e Engen
ersidade Nov
ngineering, Te
Department o
md.
dy, carried o
with the surp
ostimulation
ays showed
roleum hyd
f both techn
s in a remed
remediatio
h PHC va
of the
heating was
considered
ar with low
STRATEGIES
TING FROM
mussen2,3, P
andra B. Rib
nharia do Am
va de Lisboa,
echnical Univ
of Bioscience
out in Sisimiu
plus heating
n were also
that biostim
drocarbons
nologies was
diation strat
on trend wi
lues contin
system, ev
the best ap
a reliable o
w maintenan
S AIMING O
AN INCINE
Pernille E. J
beiro1
mbiente, Facul
Caparica, Por
versity of Den
e, Aarhus Univ
unl.pt
ut, Greenlan
g from an in
tested, in p
mulation and
(PHC) rem
s even more
egy. Howev
th all treatm
nued to d
ven at low
pproach for
ption for fas
nce and usin
OIL REMEDIA
RATION FAC
ensen2, Ma
dade de Ciên
rtugal
mark, Lyngby
versity, Roski
nd, assessed
ncineration f
arallel. An in
d active hea
moval comp
e effective, c
ver, between
ments stabi
decrease. T
w tempera
PHC remov
ster PHC rem
ng “waste‐h
Págin
ATION IN A
ACILITY
ads Højrup2
ncias e Tecnol
y, Denmark
ilde, Denmark
d the potent
facility. Indiv
nterim evalu
ating, as sep
pared to n
corroboratin
n day 42 an
ilizing excep
This shows
atures. Cou
val. The prop
moval and c
heating” fro
a | 32
ARTIC
2,
logia,
k
tial to
vidual
uation
parate
atural
ng the
d day
pt for
s the
upling
posed
can be
om an
A
Touri
relati
cases
Anta
1993
the a
explo
on ea
Kirsh
socia
Goffm
settin
socia
touri
the c
settin
board
wond
of th
and s
of ou
that l
ANTARCTIC
ism to and t
ively little co
s actual bo
rctic tourist
to almost 4
allure of Ant
ores Antarct
arlier anthro
henblat‐‐‐ Gim
ally enacted
man who su
ng where so
al life as a f
sm, there is
context of
ngs: starting
ding of a cru
derful landsc
e different
super‐‐‐huma
ur work will
leads the SC
PLOTS: TOU
through Ant
omfort, exp
dy pain. De
ts has drast
40,000 in 20
tarctica for
tic tourism a
opological w
mblett), we
theatrical p
uggested us
ocial actors p
forms of eff
s of course n
Antarctic to
g at the chec
uise ship, the
capes, and t
settings, to
an – charact
shed new l
CAR social sc
URIST PERF
David Pi
CR
pic
tarctica usua
oses tourist
espite these
ically increa
012 (IAATO,
tourists? Wh
as a cultural
works on per
e suggest an
play. We tak
s to conside
play roles, fo
fervescent d
no fixed sta
ourism, trav
ck‐‐‐in at the
e passage to
the journey
urists encou
ters that are
ight on the
cience group
FORMANCE
icard1, Denn
RIA‐‐‐FCSH/UN
CIES/ISCTE2
cccccgmail.co
ally necessit
ts to extrem
e little‐‐‐allu
ased over th
2012). How
hy would an
ly framed so
rformance in
n approach
ke up an ep
er everyday
ollow scripts
drama. In m
age setting,
vellers mov
e airport, foll
o Antarctica
back home.
unter variou
e part of the
crucial issue
p’s work.
AND THE M
nis Zuev2
NL1
om
tates a long
me weather a
ring seemin
he past 20 y
can this inc
nybody wan
ocial practic
n tourism (V
to the tou
pistemology
life in term
s and throug
most everyd
as in a conv
ve through
lowed by th
, the encoun
. On the way
us – human,
play. We wo
e of “values
MODERNITY
journey, is e
and cold, an
ng qualities,
years, passin
crease be ex
nt to travel t
ce and perfo
Victor Turner
uristic journe
y initially de
ms of a perf
gh their inter
ay life cont
ventional th
a series of
e journey to
nter of wildl
y, while eng
half‐‐‐huma
ould hope th
s” associated
Págin
Y OF NATUR
expensive, o
nd causes in
, the numb
ng from 6,0
xplained? W
there? The
ormance. Bu
r, Edward Br
ey in terms
eveloped by
formative th
ractions gen
texts includ
heatre. Inste
tourism sp
o the harbou
life, weathe
gaged within
an, almost h
hat the outc
d with Anta
a | 33
RE
offers
many
ber of
000 in
What is
paper
uilding
runer,
s of a
Ervin
heatre
nerate
ing in
ead, in
pecific
ur, the
r, and
n each
uman
comes
arctica
APRESENTA
AÇÕES
S EM PAINEL
Págin
L
a | 35
TH
P
Anta
years
forec
coast
shallo
In ex
Noto
salini
the R
to ex
8ºC u
to re
in ch
and a
No si
prelim
prote
reduc
induc
ATPa
fish a
adap
Funde
and C
Surve
HE STRESS R
ROSSII AN
Pedro M. Gu
Compa
rctic fishes
s. Recent cli
cast models
tal areas of
ow waters in
xperiments
thenia coriic
ity to evalua
Rothera (UK
xperimental
using thermo
circulating t
hanging con
agonists (de
ignificant m
minary data
eins were up
ced in fish
ced a depe
ase activity,
are reactive
ptive respons
ed by FCT‐FP
Caixa Geral d
ey and Polish A
RESPONSE A
ND NOTOTH
uerreiro, Els
arative and M
Unive
evolved in a
imate chang
s indicate th
f maritime A
n enclosed a
run in 200
ceps and N. r
ate the resp
K) and Arcto
tanks in cold
ostat‐contro
tanks, over a
ditions were
examethason
mortality or c
a shows th
pregulated a
exposed to
ndent incre
decreasing
to environm
ses may be c
(PEst‐C/MAR/
de Depósitos
Academy of S
AND OSMO
ENIA CORIIC
C
sa Couto, B
Deloffre, A
Molecular End
ersidade do A
p
a stable the
ges contribu
he rate of s
Antarctica,
areas.
05 and 201
rossii, to rap
ponse of sev
wski (PL) st
d rooms and
olled heaters
a period of u
e tested us
ne, cortisol)
changes in b
hat both co
after a heat s
o challenging
ease in plas
osmoregula
mental chan
compromise
/LA0015/2011)
s New Polar
Sciences.
OREGULATIO
CEPS EXPOS
CHALLENGE
Bruno Louro
Adelino V.M
docrinology G
Algarve, 8005‐
rmal and ha
uted to a sig
such change
possibly lea
12/13 we ex
pid but gradu
veral physio
tations using
d acclimated
s, and from
up to 10 day
ing GR/MR
, and inhibit
behaviour b
ortisol and
shock but th
g condition
ma osmola
atory efficie
nge, but tha
ed.
), FCT‐FAAC‐N
Scientists fu
ON IN ANTA
SED TO THE
ES
o, Eduarda
M. Canario
roup, Centre
‐139 Faro, Por
pt
aline environ
gnificant ris
es will incre
ading to ice
xposed two
ual changes
ological proc
g traps or fis
d from natur
32‰ to 20‐10
ys. The roles
blockers (m
ting cortisol
etween the
gene expr
hat the stres
s. Additiona
lity while d
ency. These
at their abili
Noto project,
und. Logistic
ARCTIC FISH
RMAL AND
M. Guerrei
of Marine Sc
rtugal.
nment for ro
se in water t
ease in com
e melting an
o species o
in water tem
cesses. Fish
shing poles
ral temperat
0‰ by additi
s of the stre
mifepristone,
release (usin
groups we
ession of m
ss response
ally, the rise
ecreasing b
results sho
ty to accom
FCT‐Program
support from
Págin
H NOTOTHEN
D OSMOTIC
iro, Laurenc
ciences,
oughly 30 m
temperatur
ming years i
nd fresheni
of Notothen
mperature o
collected ar
were transf
tures (0‐2ºC)
ion of freshw
ess endocrin
, spironolac
ng metyrapo
re observed
metabolic‐re
to handling
e in temper
branchial Na
ow that Ant
mmodate rap
ma Polar Port
m British An
a | 37
NIA
ce
million
e and
n the
ng of
nidae,
or/and
round
ferred
) to 4‐
water
e axis
ctone)
one).
d. Our
elated
g were
rature
a+/K+‐
tarctic
pid or
tuguês
tarctic
EF
KID
Pri
1 Ad
Ru
The t
evolv
ocea
abou
incre
enzym
eleva
Statio
8+0,5
withi
wher
able t
To fin
four
dehy
day a
occur
upreg
(4°C)
nega
were
and L
conc
*prese
Unive
FFECTS OF T
DNEY OF AN
iscila Krebsb
Flávia Bad
daptative Biol
a Coronel Fra
2 Departme
Campus d
thermal sta
ve efficientl
ns in partic
ut the meta
asing temp
mes of ene
ated temper
on (EACF) a
5°C for 1, 4,
in the avera
re the fish w
to induce m
nd out how
enzymes:
ydrogenase (
at 4°C e 8°C,
rred upreg
gulation of C
maintained
tive modula
e lower leve
LDH did not
lusive, beca
ently at Compa
ersidade do A
TEMPERATU
NTARCTIC T
bach1, Tânia
duy Vaz da S
ogy Laborato
ancisco Herac
nt of Biology,
do Bom Conse
bility of the
y their met
cular around
bolic plastic
erature. Th
rgy metabo
rature. The
and both sp
15 and 30 da
age of the t
were caught
metabolic cha
w fishes were
glucose‐6
(MDH); and
and 15 days
ulation at
CS and LDH
d for 15 days,
ation in subj
ls of CS and
t vary signif
use process
rative and Mo
Algarve, 8005‐
URE ACCLIM
TELEOSTS N
a Zaleski1, Cin
Silva1,*, Lucia
Rodrigu
ory, Departme
clito dos Sant
, Basic Institu
elho, Rua 04 d
pkre
e Antarctic
tabolism at
d the Antarc
city and acc
us, this stu
olism in Noto
experiment
pecies were
ays. The tem
thermal var
t. Already w
anges and 8
e able to su
6‐phosphata
lactate deh
s at 4°C led t
4° C comp
compared w
, and for ind
jects acclima
d MDH as a
ficantly in r
ing and ana
olecular Endo
‐139 Faro, Por
MATION ON
NOTOTHENIA
ntia Machad
ana Badeluk
ues2, Lucélia
ent of Cell Bio
tos, 210, Centr
Brazil
ute of Bioscie
de Março, 43
bsbio@gmai
marine eco
low tempe
ctic Peninsu
climation ca
dy investiga
othenia ross
ts were perf
exposed to
mperature o
iation found
warming at 4
8°C is close to
urvive in the
ase (G6Pas
hydrogenase
to lower lev
pared with
with the co
dividuals acc
ated at 8 ° C
result of he
renal tissue
lysis are ong
ocrinology Gr
rtugal.
ENERGY M
A ROSSII AN
do1, Maria R
k Cettina1, M
Donatti1
ology, Federa
ro Politécnico
nces, Univers
2, CEP 12020‐
l.com
osystem has
eratures. Ho
ula and adja
pacity of th
ated the lev
sii and Notot
formed at C
o temperatu
of 0°C was ch
d in Admira
4°C is an exp
o the therm
ese conditio
se); citrate
e (LDH). The
els of G6Pas
8°C. The h
ntrol group
climated at 4
C for 4 days
eating (4°C).
of N. coriice
going.
oup, Centre o
METABOLISM
D NOTOTHE
Rosa Dmeng
Mariana Forg
al University o
o, CEP 81531‐9
sity of Taubat
270, Taubaté
allowed An
owever, the
acent islands
he Antarctic
vels of activ
thenia coriic
Comandante
ures of 0+0,
hosen as a c
lty Bay, Kin
perimental t
al tolerance
ns, we teste
e synthase
e acclimation
se in kidney,
heating in 8
and the exp
4°C for 30 da
s. While in N
. The tissue
eps. The dat
of Marine Scie
Págin
M ENZYMES
ENIA CORIIC
geon Pedrei
gati1, Edson
of Paraná – U
970, Curitiba,
té – UNITAU,
é, SP, Brazil
ntarctic fish
warming o
s raise ques
c notothenio
vity of som
ceps subject
e Ferraz Ant
,5°C, 4+0,5°C
control, sinc
ng George Is
thermal con
e of Antarcti
ed the activ
e (CS); m
n of N. rossi
, while at 30
8°C induced
perimental g
ays. The MD
N. coriiceps,
levels of G6
ta so far ar
ences,
a | 38
S IN
CEPS
iro1,
FPR,
PR,
hes to
of the
stions
oid to
e key
ted to
tarctic
C and
ce it is
sland,
dition
c fish.
vity of
malate
ii for 1
0 days
d the
group
H had
there
6Pase
re not
EC
R
Ga
Cin
1 Ad
Ru
Know
the e
supp
same
the m
collec
Island
juven
chara
follow
due
obse
and
great
glyco
comp
term
moni
*prese
Unive
COLOGICAL A
OSSII AND N
abriela Raga
ntia Macha
daptative Biol
a Coronel Fra
2 Departme
wing the bio
ecological in
orts the kn
e system by
metabolism
cted at a d
ds, Antarctic
niles, and th
acterised as
wed by mac
to the con
rved in the
ages attain
ter total con
ogen and to
ponents did
analysis of
itor the spec
ently at Compa
ersidade do A
AND PHYSI
NOTOTHENI
a¹; Helen A
ado¹, Edson
ogy Laborato
ancisco Herac
nt of Biology,
logy and eco
teractions a
owledge of
different sp
and diet of
depth of up
c Peninsula.
hat of N. co
bentho‐pla
croscopic alg
stancy of t
hepatosom
ed by this
ncentration
otal lipids w
not exhibit
the biologi
cies present
rative and Mo
Algarve, 8005‐
OLOGICAL A
IA CORIICEPS
udrey Pichl
Rodrigues
Rios¹;
ory, Departme
clito dos Sant
, Basic Institu
do
ology aspec
among these
f mechanism
pecies. This
f the Antar
25 m in A
The popula
oriiceps (n=1
anktivorous
gae. The ab
the diet du
matic index o
species. Am
of protein w
were most a
seasonal pa
cal paramet
in Admiralty
olecular Endo
‐139 Faro, Por
ASPECTS O
S IN ADMIR
ler¹; Tânia Z
s2, Helena G
; Lucélia Do
ent of Cell Bio
tos, 210, Centr
Brazil
ute of Bioscie
onatti@ufpr.
cts of Antarc
e organisms
ms that enab
work aimed
rctic fish No
Admiralty Ba
ation structu
151) was co
and the sal
bsence of se
ring the st
of N. coriice
mong the e
was observe
abundant in
atterns but
ters evaluat
y Bay, a regi
ocrinology Gr
rtugal.
F THE ANTA
RALTY BAY,
Zaleski¹, Fla
Gonçalves K
onatti1
ology, Federa
ro Politécnico
nces, Univers
.br
ctic fish may
s. Furthermo
ble coexiste
d to evaluat
otothenia ros
ay, King Geo
ure of N. ros
omposed of
ps were the
easonality in
udy period.
ps and was
energetic co
d in the mu
the livers o
displayed la
ed in this st
ion with gre
oup, Centre o
ARCTIC FISH
ANTARCTIC
via Baduy V
Kawall3, Flav
al University o
o, CEP 81531‐9
sity of Taubat
help in the
ore, provide
ence and ex
te the temp
ssii and Not
orge Island,
ssii (n=221) w
adults. The
e dominant
the fitness
. The great
related to
onstituents o
scles of N. c
of both spe
arge monthly
tudy should
at biologica
of Marine Scie
Págin
H NOTOTHE
C PENINSUL
Vaz da Silva
via Sant’An
of Paraná – U
970, Curitiba,
té – UNITAU,
understand
information
xploitation o
poral variatio
tothenia cor
, South She
was compos
ese species
item in the
factor was
ter variation
the greater
of the tissu
coriiceps, wh
ecies. The p
y variation.
d be continu
l diversity.
ences,
a | 39
ENIA
LA
a¹*,
nna
FPR,
PR,
ing of
n that
of the
ons in
riiceps
etland
sed of
were
e diet,
likely
n was
r sizes
ues, a
hereas
lasma
Long‐
ued to
TH
FRO
J
1 Inst2 Na
The c
and
collec
areas
stom
impo
estim
due t
the c
other
latitu
with
isoto
forag
had d
varie
betw
differ
struc
know
HE ROLE OF
OM PREDAT
José Seco1,
titute of Marin
atural Institut
3 British An
cephalopod
Antarctic t
cted betwe
s with ove
machs and i
ortant cepha
mated mass)
to oceanic f
cephalopod
r locations
ude. We can
a South Ge
opes ratios o
ging areas o
different pr
s according
ween adults
rent prey.
cture around
wn area of th
F CEPHALOP
TORS DIET (
Jim Rober
ne Research,
e of Water an
14
ntarctic Surve
componen
toothfish D
en March t
rlapping po
in 77% of D
alopod spec
) and on D. e
fronts, the c
component
we found
n also see s
orgia study
of nitrogen
of cephalopo
rey and com
g to prey av
and sub‐‐‐a
Our study
d South San
he Southern
PODS AROU
(DISSOSTICH
AND S
ts2, Filipe C
Guerreiro
Department
nd Atmosphe
‐‐‐901, Kirbirn
ey, NERC; High
joses
t on the di
issostichus
o April 200
opulations.
D. mawsoni
cies by esti
eleginoides (
cephalopods
t on the die
different d
ignificant di
(both archi
(δ15N) and
ods, respect
mpared with
vailability. T
dults of K.
provides v
dwich Island
Ocean.
UND SOUTH
HUS ELEGIN
STABLE ISO
Ceia1, Alexan
o1 and José
of Life scienc
eric Research,
nie, Wellingto
h Cross, Mad
s.seco@gmai
et of Patag
mawsoni w
9 around S
Cephalopo
stomachs.
mated mas
(89%). Despi
s species pr
et of toothfi
distribution
ifferences o
pelagos are
carbon (δ13
tively. The δ
h other stud
The δ13C de
longimana a
valuable info
ds as well as
SANDWICH
OIDES AND
OTOPES
ndra Baeta1
C. Xavier1,2
ce, University
, 301 Evans Ba
on, New Zeala
ingley Road,
il.com
gonian tooth
were analys
outh Sandw
ds occurred
Kondakovia
s on D. ma
te the segre
eyed were a
sh around S
of cephalop
on vertical d
e in the Scot
3C) we can
δ15N indicat
dies show th
emonstrate
as also that
ormation fo
s the role of
H ISLANDS:
DISSOSTICH
1, Pedro Alv
y of Coimbra,
ay Parade, Gre
and
CB3 0ET, Cam
hfish Dissost
ed from st
wich Islands,
d in 24% o
a longimana
awsoni (96%
egation of th
almost the s
South Sandw
pods specie
distribution
tia Sea). Ana
assess the
e that adult
hat the diet
a clear spe
t cohabiting
or the Anta
f cephalopo
Págin
INFORMAT
HUS MAWSO
vito1, Migue
Coimbra, Por
reta Point, PO
mbridge, UK
tichus elegin
tomach sam
, one of the
of D. elegin
a was the
% of cephalo
he two toot
same. Comp
wich Islands
es dependin
when comp
alysing the s
trophic leve
ts and sub a
t of cephalo
ecial segreg
g species fee
arctic food
ods, in that p
a | 40
ION
ONI)
el
rtugal
O Box
noides
mples
e few
noides
most
opods
thfish,
paring
s with
ng on
paring
stable
el and
adults
opods
gation
ed on
web
poorly
T
Sa
1 2
4 CE
Cont
is aff
high
envir
forag
conc
accum
conc
Geor
Weig
had
anim
such
levels
levels
TEMPORAL
ara Pedro1, J
Centre of Fu2 Institute of M
3 British An
ESAM (Centre
amination c
fecting remo
toxicity an
ronment. As
ge nearby th
entrations
mulated ann
entrations i
rgia. Mercur
ght influence
significant
als eat bigg
as egg‐layin
s over 10 ye
s closer to th
AND INTRA
GE
José C. Xav
E
nctional Ecol
Marine Resea
ntarctic Surve
e for Environm
caused by an
ote areas su
nd capacity
s Gentoo p
heir colonies
in the reg
nually, as th
n Gentoo p
ry levels ran
ed mercury l
higher mer
ger prey and
ng. Comparin
ears. There w
he Antarctic
ASPECIFIC V
NTOO PENG
vier2,3, Sílvia
Eduarda Pe
ogy, Departm
arch, Departm
ey, NERC, Hig
mental and M
Aveiro, 38
saralm
nthropogeni
uch as Antar
y to biomag
penguins (Py
s, they are e
gion. Their
he moult occ
penguin feat
nged from 0
evels, with b
cury levels
d that femal
ng to other
was spatial v
c continent.
VARIATIONS
GUINS, PYG
a Tavares1, N
ereira4 & Mi
ment of Life S
ment of Life S
gh Cross, Mad
arine Studies
810‐193 Aveiro
ondega@gm
ic activities
rctica. Mercu
gnify throu
ygoscelis pa
expected to
feathers c
curs every y
thers, of kn
0.15 to 3.10
bigger peng
than fema
les have ext
studies, the
variation in
S OF MERCU
OSCELIS PAP
Norman Ra
iguel Parda
ciences, Univ
ciences, Univ
dingley Road,
s) & Departme
o, Portugal
mail.com
has increase
ury is one of
ugh food w
apua) breed
o be a good
can indicate
year. In this
own sex an
mg kg‐1, w
guins having
les. These
tra routes fo
ere was no t
this species
URY ACCUM
PUA
atcliffe3, Ph
l1
versity of Coim
versity of Coim
CB3 0ET Cam
ent of Chemis
ed over the
f these cont
webs is of
d all around
bioindicato
e the amo
study we ev
nd size, in B
ith a mean
higher merc
results sugg
or eliminatin
emporal var
, with a dec
Págin
MULATION I
il N. Tratha
mbra, Portug
mbra, Portug
mbridge, UK
stry, Universi
last decade
taminants a
concern to
d Antarctica
or of the me
ount of me
valuated me
Bird Island, S
of 0.95 mg
cury levels.
ggest that b
ng contamin
riation in me
crease in me
a | 41
N
an3,
al
al
ity of
es and
nd its
o the
a and
ercury
ercury
ercury
South
g kg‐1.
Males
bigger
nants,
ercury
ercury
I
N. V
3 Ce
5 I
Unde
adap
ecosy
recog
ecosy
comp
biom
Infor
consu
preda
partic
feedi
38° W
their
resul
gaud
Gent
Anta
with
strug
later.
the A
be af
NTRA‐ANN
Velez1, N. Ra
2 B
entre d´Etude
4 Royal Belg
nstitute of M
erstanding t
pt to environ
ystems. In
gnised as be
ystems to c
ponent of th
mass and pla
rmation on
umption mo
ator behavi
cularly durin
ing ecology
W) during th
diets, popu
ts in the
ichaudii wa
oo penguin
rctic Winter
apparently
ggled. This w
. In terms o
Antarctic Win
ffected.
UAL VARIAT
PAPUA) A
atcliffe2, P.
1 University
British Antarct
e Biologique d
gian Institute
Inv
Marine Resear
he natural v
nmental cha
the Southe
eing importa
change due
he Antarctic
y an import
the diet a
odels in Anta
iour could a
ng the Anta
of gentoo p
he Antarctic
ulation dyna
conservatio
s the main
ns diets we
r. As environ
lack of Anta
was expresse
of conservat
nter in this r
TIONS OF T
AT SOUTH
N. Trathan
K. Erzin
y of Algarve, F
tic Survey, Hi
de Chizé, UPR
UBP 14, 793
for Natural S
vertebrates, R
ch (IMAR‐CM
corde
variability of
ange, is cruc
ern Ocean,
ant in determ
to climate
marine ecos
tant role, as
and feeding
arctic food w
adapt over
arctic Winte
penguins Py
Winter of 2
amics of the
on of these
prey of Ge
re able to
nmental con
arctic krill Eu
ed in their a
ion, if these
region, the p
THE DIET O
GEORGIA (
2, G. Tarling
ni1 and J. C. X
FCMA, Gambe
gh Cross Mad
R 1934 du Cen
60 Villiers en
Sciences, Labo
Rue Vautier 29
MA), Universit
egeleia@gma
a marine ec
cial to the co
the netwo
mining the r
or fisheries
system, con
s consumers
g ecology
webs. Furthe
the long t
er (June‐ Se
ygoscelis pap
2009, using
eir most abu
e penguins.
entoo peng
show the g
nditions see
uphausia sup
ttempt to b
e unfavoura
population o
F GENTOO
SOUTHERN
g2, Y. Chere
Xavier2,5
elas, 8000 Fa
dingley Road,
ntre Nationale
Bois, France
oratory of Car
9, 1000 Bruxe
ty of Coimbra
ail.com
cosystem, an
onservation
ork of food
resilience an
s. Penguins
nstituting ap
s, on the top
of penguin
ermore, it is
term to exp
eptember).
pua at Bird
scats to as
undant prey
. Suprisingl
uins (presen
growth of T
emed unfavo
perba in clos
breed in the
ble conditio
of Gentoo pe
PENGUINS (
OCEAN)
l3, C. Broye
ro, Portugal
, Cambridge,
e de la Recher
rcinology, De
elles
, 3001‐401 Co
nd how orga
and manag
d web inte
nd hence res
(Spheniscid
proximately
p of the Ant
ns is vital
s currently u
ploit alterna
In this stud
Island, Sout
sess intra‐an
and conseq
y, the amp
nt in 77.1%
T. gaudichau
ourable to G
se by waters
following Su
ons continue
enguins in S
Págin
(PYGOSCEL
er4, F. C. Gar
UK
rche Scientifi
epartment of
oimbra, Portug
anisms are a
gement of m
eractions is
sponse of m
dae) are a
y 80% of the
tarctic food
to parame
nknown wh
ative prey t
dy we asses
th Georgia (
nual variatio
quences of
phipod The
of the sam
udii throug
Gentoo peng
s, these pen
ummer 2‐3 w
e to occur d
South Georg
a | 42
IS
rcia1,
que,
gal
ble to
marine
now
marine
major
avian
web.
terise
hether
types,
ss the
(54° S,
ons in
these
emisto
mples).
h the
guins,
nguins
weeks
during
ia can
OCE
L
2 La
3 In
In
Ocea
comm
unde
surfa
Macr
Stink
There
Dens
There
signif
differ
nega
poten
prod
mean
enha
male
use a
forag
at St
distri
chara
than
sugg
prod
EANOGRAPH
Lucas Krüger
1 Instituto d
boratório de
nstituto Naci
nstituto de B
anographic
munities, bu
erstood. We
ace tempera
ronectes giga
ker Point at
e were no d
sities (KD) sh
e was a tend
ficant negat
rences in Ch
tively assoc
ntial avoida
uctivity, bec
ns that in ar
nced. This i
s are more
a dual coas
ging strategy
tinker point,
ibution, but
acteristics. W
that follow
ests that co
uctivity.
HIC CHARAC
r1,3*, Jaime A
do Mar, Centr
Univ
e Ornitologia
ional de Ciên
Biologia, Cen
factors ar
ut how gend
e evaluated
ture (SST) o
anteus durin
t Elephant I
differences in
howed a sig
dency of fem
tive relation
hl‐a and SST
ciated with
ance of ma
cause the gr
reas with hi
is a species
aggressive
stal‐pelagic
y and female
, difference
t detailed
We suggest t
wed by mal
ompetition b
CTERISTICS T
HABITAT
A. Ramos1, Jo
ro do Mar e d
versidade de
a e Animais M
Le
cia e Tecnolo
ntro de Ciênc
Janeiro,
lkg
re importa
ders use fora
the influen
on the differ
ng the aust
sland, Mari
n latitude an
nificant diffe
males to avo
nship betwe
T used by b
SST while m
ale core ar
eater the co
igh marine
whose activ
and more e
foraging m
es assume a
s were not
habitat use
that females
les to avoid
between ma
TO EXPLAIN
TS BY GIANT
osé Xavier1,
do Ambiente
e Coimbra, Co
Marinhos, Un
eopoldo, Bra
ogia Antártic
cias da Saúde
Rio de Janei
nt in exp
aging habita
nce of Chlo
rential habit
tral summer
itime Antarc
nd longitude
erence in th
oid the core
een the KD
both sexes,
male KD wa
reas by fem
oncentration
productivity
ve interfere
efficient in f
mode but m
a predomina
that clear
e was char
s adapted by
d competiti
les and fem
N SEXUAL S
T PETRELS
Vitor H. Paiv
e, Departame
oimbra, Port
niversidade d
asil
co de Pesqui
e (CCS) Unive
ro, Brasil.
c.pt
plaining the
ats and redu
orophyl‐a co
tat use by m
r. We tagge
ctic Peninsu
e of sites us
e core areas
areas used
of males a
but we det
as positively
males could
n of Chl‐a the
y, the femal
ence betwee
foraging on
males assum
antly pelagic
and both se
racterized b
y following d
ion with th
ales is lowe
SEGREGATIO
va1, Maria Vir
ento de Ciên
ugal.
do Vale do Ri
sas Ambient
ersidade Fed
e organizat
uce competit
ncentration
male and fem
d 7 females
ula, with Lo
ed by both s
s used by m
by males, c
and females
tected that
y associated
d be attrib
e lower was
e and male
en sexes is
coastal carr
me a predo
foraging st
exes overla
by differen
different en
em. As exp
r in areas w
Págin
ON IN FORA
rginia Petry2
ncias da Vida,
io dos Sinos,
tais – INCT‐A
deral do Rio d
tion of se
tion is still p
n (Chl‐a) an
male Giant P
s and 11 ma
otek geoloc
sexes, but K
ales and fem
corroborated
s. There we
females KD
d with Chl‐a
buted to m
s the avoidan
e KD relation
possible be
rions. Both
ominantly co
rategy. How
pped in for
nt oceanogr
nvironmenta
pected, our
with higher m
a | 43
AGING
2,3
,
São
PA,
de
eabird
poorly
d sea
etrels
ales in
ators.
Kernel
males.
d by a
re no
D was
a. The
marine
nce. It
n was
cause
sexes
oastal
wever,
raging
raphic
l cues
r data
marine
W
Luc
1 IMA
2 La
3 In
In
While
of So
their
recen
prob
evalu
Marit
non‐b
Petre
the 6
(Chl‐a
South
ice‐ed
1.5 m
winte
speci
niche
Furth
popu
WHERE DO
PET
cas Krüger1,3
AR‐CMA Cent
boratório de
nstituto Naci
nstituto de B
e migration
outhern Gian
home rang
nt data from
ably use bo
uated the y
time Antarc
breeding ho
els foraging
60ºS parallel
a 0.6±0.01 m
h America d
dge at consi
m) waters. T
er. It confirm
ies, and also
e during the
her analysis
ulations rega
THEY GO?
TRELS FROM
*, Elisa de S
ro do Mar e
e Ornitologia
ional de Ciên
Biologia, Cen
is a commo
nt Petrels (M
ge during wi
m stable isot
oth Antarct
year round
ctic Peninsul
ome range
in cold (0.6
l during the
mg/m3), shal
during the no
iderably low
This behavio
ms former h
o contribute
e non‐breed
should cont
arding their t
DOES YEAR
M ANTARCT
ouza Peters
Mari
do Ambiente
Coimbra
a e Animais M
Le
cia e Tecnolo
ntro de Ciênc
Janeiro,
lkg
on behavior
Macronectes
inter but wi
ope analysis
tic and Sub
movements
a using geo
habitats. W
6±0.04ºC) m
breeding se
low (223 ± 1
on‐breeding
w productive
or generate
hypothesis f
es to unders
ing period d
tribute to de
trophic nich
R‐ROUND M
TICA REVEA
sen2,3, Jaime
ia Virginia Pe
e, Departam
a, Coimbra, P
Marinhos, Un
eopoldo, Bra
ogia Antártic
cias da Saúde
Rio de Janei
for many se
s giganteus)
ithout chang
s suggests t
bantarctic w
s of a Sout
olocation me
We found a
mid‐producti
eason, and
14 m) and te
g season, ho
e (Chl‐a 0.15±
ed a bimod
for the mov
stand why t
due to the
eepen our un
he, relations
MOVEMENT
AL A MIGRA
A. Ramos1, J
etry2,3
mento de Ciên
Portugal.
niversidade d
asil
co de Pesqui
e (CCS) Unive
ro, Brasil.
c.pt
eabird speci
) appear to
ging the cen
hat Antarct
waters throu
hern Giant
ethods, and
clear spatia
ve (Chl‐a 0.
then using p
emperate (6
owever, the
±0.002 mg/m
al home ra
vements of
the Souther
exploration
nderstandin
with fisherie
TS OF SOUT
ATION PATT
José Xavier1,
ncias da Vida
do Vale do Ri
sas Ambient
ersidade Fed
es, Subanta
be resident
nter of disp
ic Populatio
ughout the
Petrel popu
describes t
al shift, with
5±0.01 mg/m
preferential
.1±0.02ºC) w
birds made
m3) and sligh
nge and ha
Antarctic p
rn Giant Pet
of distinct
g of the eco
es and clima
Págin
THERN GIAN
ERN
, Vitor H. Pa
a, Universida
io dos Sinos,
tais – INCT‐A
deral do Rio d
arctic popula
t, only incre
ersion. How
ons of this sp
year. Our
ulation from
the breedin
h Southern
m3) waters
ly the produ
waters near
incursions t
htly deeper (
abitat use d
population o
trels have a
habitat fea
ology of Ant
atic change.
a | 44
NT
iva1,
de de
São
PA,
de
ations
easing
wever,
pecies
study
m the
g and
Giant
south
uctive
south
to the
(392 ±
during
of this
large
tures.
tarctic
CLI
Cata
1 Cen
2 M
Distribution
Global tem
colonizatio
differentiat
related env
differences
effects on
functioning
distribution
temperatur
the seagra
approach u
expression
resistance,
support fo
leading an
distribution
detected a
expected th
IMATE CHA
AT TH
rina Mota1*
ntro do Ciênc
editerranean
(CSI
n patterns
mperature inc
ns. These s
ted populati
vironmenta
s of fitness‐r
ecosystem
g impact. We
nal leading
res between
ss Zostera m
using photo
study to t
respectivel
r the hypot
nd trailing e
nal edge of F
at temperatu
hat their ran
ANGE EFFECT
HEIR LEADI
*, Aschwin
cias do Mar (C
Cam
Institute for
C) – Universit
*
of marine
crease is ex
shifts depen
ions. Popula
l change. D
related trait
m structurin
e tested the
and rear r
n leading an
marina. In c
synthetic in
test the res
ly, of leadin
thesis that d
edges. Fitne
F. vesiculosu
ures beyond
nge will expa
TS ON ECOS
NG POLAR A
H. Engelen
Ester Serr
CCMAR), CIMA
mpus de Gam
Advanced St
ty of the Bale
*these author
aengelen@
organisms a
xpected to r
ndent on d
ations at the
Despite rese
s in leading
ng species
e hypothesis
range edges
nd rear edge
common ga
ndicators wa
silience to e
ng and rear
differentiati
ess at elev
s relative to
d those pre
and northwa
SYSTEM ST
AND REAR
1*, Márcio C
rão1, Gareth
AR‐Laboratór
belas, 8005‐1
tudies (IMEDE
earic Islands (
rs share equa
@ualg.pt, cfmo
are mainly
result in dist
emography
e limits of dis
earch effort
versus rear
are expect
s that fitnes
s, by comp
e population
rden exper
as combined
elevated se
r edge pop
on of therm
vated temp
o southern p
edicted for t
ards with glo
TRUCTURING
EDGE DIST
Coelho1, Car
h Pearson1
rio Associado
39 Faro, Port
EA), Spanish C
UIB), Esporle
al responsibilit
determined
tribution shi
and adapt
stribution ar
ts, little is
r edge range
ted to have
ss and adapt
paring respo
ns of the se
iments, a co
d with a hea
awater tem
pulations. O
mal stress re
eratures wa
opulations.
the polar re
obal change
G MARINE M
RIBUTION Z
rlos Duarte
o FCT, Univers
tugal
Council for Sc
es, Mallorca, S
ty
d by seawat
fts and loca
tive evolutio
re at the fore
known abo
e population
e the stron
tive potentia
onses to ele
aweed Fucu
omparative
at shock pro
mperatures,
ur results p
esponse can
as eroded
Temperatur
egion in the
e.
Págin
MACROPHY
ZONES
e2, Núria Ma
sidade do Alg
cientific Rese
Spain
ter tempera
al extinction
on of gene
efront of cli
out perform
ns. Global ch
ngest ecosy
al differ bet
evated seaw
us vesiculosu
ecophysiolo
otein (Hsp)
and the re
provide emp
n occur bet
at the nor
re stress wa
e future, and
a | 45
YTES
arbà2,
garve,
arch
ature.
ns and
tically
mate‐
mance
hange
ystem
tween
water
us and
ogical
gene
elative
pirical
tween
rthern
s only
d it is
Joa
1 Cen
2 De
The D
dries
comm
quest
cyclin
sever
have
focus
In th
Valley
prog
km2 i
were
camp
envir
differ
vege
NITR
archa
varia
critic
envir
chan
NITROEX
ana Séneca1
ntre of Marine
epartment of B3 College of
Dry Valleys o
t desert o
munities, wh
tions on the
ng and ecolo
ral field exp
been perfo
sed in evalua
is poster we
y, under the
ram. The 20
n Victoria V
e set up to c
paign, with
ronmental f
rent scientif
tation analy
OEXTREM p
aea and ba
bles that are
al findings
ronments, an
ges in polar
XTREM: 20
1, Maria Mo
e and Environ
Biological Scie
Earth, Ocean
of Eastern A
on Earth. T
hich are beli
eir diversity,
ogical proce
peditions to
ormed on be
ating the bio
e present th
e NITROEXT
013 Antarctic
Valley and su
cover a tota
the main go
factors. Sam
fic proposes
ysis by integr
project, sam
cteria nitrif
e responsibl
to understa
nd a better
ecosystems
013 ANTARC
onteiro1, Hu
Ste
mental Resea
4050‐
ences, Univers
and Environm
joanas
Antarctica a
The severit
eved to driv
, abundance
esses remain
the Dry Va
ehalf of an
ocomplexity
he past expe
TREM projec
c field camp
urrounding
al of 86 rand
oal of buildi
mples collec
s, like invert
rating interd
mples will b
iers, as wel
le for their d
and the dyn
understandi
s, as global c
CTIC FIELD C
ugo Ribeiro
ephen C. Ca
arch, Universit
‐123 Porto, Po
sity of Waikat
ment, Universi
seneca @gma
re vast, ice‐
ty of such
ve all proces
e, activity, a
n unanswer
alleys’ region
ongoing Ne
y of the Anta
edition to A
ct (Propolar
paign covere
areas. One
dom samplin
ing a model
cted within
tebrate, geo
disciplinary c
be processe
ll as comm
distribution.
namics of t
ing on how
climate chan
CAMPAIGN
1, Lee Charl
ry2,3
ty of Porto, Po
ortugal
to, Private Bag
ity of Delawar
ail.com
‐free regions
conditions
ses in the sy
nd their con
red. In order
n of southe
ew Zealand‐b
arctic Dry Va
Antarctica in
r), integrate
ed a samplin
main field
ng locations
to link biod
the 86 ran
ochemical, c
complement
ed for the
unity dynam
We believe
the nitrogen
these micro
nges.
TO THE DR
les2, Catarin
ortugal, Rua d
g 3105, Hamilt
re, Lewes, Del
s believed to
s shaped u
ystem; howe
ntribution to
r to answer
rn Victoria
based intern
alleys (ICTAR
January 20
ed in the ICT
g area of ap
camp and t
s during thre
diversity wit
ndom tiles,
cosmo‐datin
tary studies.
diversity an
mics and th
that this pr
n cycle in p
obial commu
Págin
RY VALLEYS
na Magalhã
dos Bragas, nº
ton, New Zeal
laware, USA.
o be the co
unique mic
ever fundam
o biogeoche
these ques
Land, Antar
national pro
R–www.icta
13 to the Vi
TAR interna
pproximatel
three sub c
ee weeks of
th landscap
were use
ng, microbia
. On behalf o
nd abundan
he environm
roject will pr
permanently
unities respo
a | 46
S
ães1,
289,
land.
oldest,
robial
mental
emical
stions,
rctica,
ogram
ar.aq).
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ARCTICA FR
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SPORT OF A
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Págin
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tine environm
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a | 48
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e CONTANTA
nmental (lak
Deception Is
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data, all th
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TERIZATION
OF MAGMA
os1, André M
aboratório Na2 Instituto
pedro
hetland Isla
border of th
duction zon
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s also envis
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ociated to
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ARC project
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N OF DECEPT
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TION ISLAN
ATED TO RE
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S: IMPLICAT
CANISM
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h tectonic s
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a | 49
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of the distri
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models show
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WO ERT PRO
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io Correia1,
Geofísica de É
studos Geogr
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projects PER
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tivity tomog
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are conside
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raphy 40 e
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ty values (a
of electrica
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m long.
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As a prelimi
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o year. At th
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tches are, th
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plain the exi
OFILES DON
TICA) DURI
João Roch
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ráficos, Unive
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2 (Permafro
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tion of perm
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E IN A CAL
ING A PERIO
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Peninsula o
2009, 2012,
mafrost in th
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ated in the y
were used
e RES2DINV
ectrical resis
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l resistivity
vity values in
retation, in s
or sporadic
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melted wh
ting as an in
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LM SITE IN
OD OF FIVE
o Vieira2
ora, Portugal
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mate Change
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e area.
directions i
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years 2012 an
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stivity pseu
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of the grou
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some zones
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Págin
LIVINGSTO
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al
te Change i
e in the Mar
in a Circum
n Island, nea
with the obje
in the CALM
iles done in
nd 2013. For
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und to dept
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a | 50
N
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2009
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ation;
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) into
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THE HOLOCE
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ENE DEGLAC
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Dermot Anto
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cultad de Cien
Institute of E
ue Natural De5 Centre d'
de Estudios y
a is an ice‐fr
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a. During the
o reconstruct
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the first rad
ese datings,
Holocene. D
id already s
bottom sedi
ocene age,
on Peninsula
CIATION OF
CTICA) BAS
oniades2, S
abes5, Man
raphy and Sp
ncias, Univers
Earth Science
Peñalara, Ce
'Estudis Avan
y Experiment
oliva_
ree area loca
Antarctica).
e field camp
t the palaeo
n this comm
iocarbon da
, the onset
uring this p
tart, meanin
ments of lak
which sugg
a.
F BARTON P
SED ON LAC
. Giralt3, Jo
nuel Toro6 &
patial Planning
sidad de la Re
s Jaume Alme
entro de Inves
nçats de Blane
tación de Obr
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ated in the S
Numerous
paign of Jan
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munication w
ates from the
of the degl
period lacust
ng that they
kes distribut
gests small g
PENINSULA
CUSTRINE R
oão Agrela1,
& Gonçalo V
g, University
epública, Mon
era (CSIC), Ba
stigación y Ge
es (CEAB), Bla
ras Publicas (C
o.com
SW corner o
lakes forme
nuary‐Februa
ntal conditio
we present t
e base of fiv
aciation in
trine sedime
y were ice‐fr
ted next to
glacier fluct
(KING GEO
RECORDS
Ignacio Gr
Vieira1
of Lisbon, Po
ntevideo, Uru
arcelona, Spa
estión, Madrid
anes, Spain
CEDEX), Madr
of King Geor
ed following
ary’12 we co
ons and infe
he prelimina
e cores.
Barton Peni
entation in t
ree. By cont
the present
tuations dur
Págin
ORGE ISLAN
ranados4, S
ortugal
uguay
ain
d, Spain
rid, Spain
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g the deglac
ored five of
er the calend
ary results o
insula dates
the lakes lo
trast, radioca
t‐day glacier
ring the las
a | 51
D,
ergi
South
iation
these
dar of
of this
s back
cated
arbon
r front
t two
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are t
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ework of p
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intervals.
from 2009
mest year be
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suggests a
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typical of a
ailing wind d
ds from NE
age hourly w
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itions. It wil
in longer clim
NDITIONS I
KLIMENT OH
al station h
ctic Station
project PER
tation is ma
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mafrost. The
el the groun
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mo‐hygrome
arometer (CS
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orge Island)
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have been t
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wind speeds
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ands, such a
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mate data se
N THE VICIN
HRIDSKI (HU
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has been in
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RMANTAR (
intained by t
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imilar tempe
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mest month,
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time climate
re from NE t
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of 110 km/h
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s Bellingsha
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NITY OF TH
URD PENINS
Carla Mora
OT University
mora@campu
nstalled in t
eninsula (Li
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the Universi
ture monito
ctive of the s
egime and p
b near the th
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60), a wind
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mera (Harb
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us regional
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with means
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to N and fro
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ausen, Ferra
ommon regio
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thin the reg
HE BULGARI
SULA, LIVIN
a
of Lisbon
us.ul.pt
the vicinity
vingston Isl
and climat
ity of Lisbon
oring, belong
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on a Campb
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ckness sens
d by snow t
ortronics sy
mperatures
ditions were
rom ‐2.9 to ‐
climate sig
‐12.3 ºC and
air temperat
s from ‐7.7 to
by a small
om SW to S,
ts are relativ
n recorded.
ented and co
z and Juban
onal signal a
of observatio
ional climate
AN ANTARC
NGSTON ISLA
of the St
and) in Jan
te change
n and is insta
ging to the
provide me
distribution i
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sor (SR50A)
temperature
ystem). Data
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e recorded a
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d maxima fr
tures from 0
o ‐4,4ºC. The
annual tem
with strong
vely frequen
ompared to
ny. This com
and those in
ons from St
e variability.
Págin
CTIC STATIO
LAND)
Kliment Oh
nuary 2009 i
in the Mar
alled close to
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eteorologica
in the region
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ese tempera
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gest average
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nfluenced by
Kliment Oh
.
a | 52
ON
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in the
ritime
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estrial
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ude of
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meter
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ttons)
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CTS ON GRO
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ence in relat
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OUND TEMP
DECEPTION
erreira1, Mi
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alice.fe
thermal re
uctivity, mo
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et. GST var
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pose of eva
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values for l
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e and wher
imatic scale
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PERATURES
N ISLAND, A
iguel Ramo
gráficos, IGOT
ca, Universida
rreira@camp
egime are m
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frost areas
ulating effec
controlled b
ries extensi
graphy, snow
ception islan
aluating mic
talled, com
tmosphere a
and ground
afrost (TTO
croclimatic c
y altitude an
he control
low altitude
0 cm. TTO
re the morph
e allowed a
OP. The res
nderstand pe
S ALONG A V
ANTARCTICA
os2, Gonçalo
T, Universida
ade de Alcalá
pus.ul.pt
mainly cont
surface con
, winter s
ct (Ballantyn
by complex e
ively in spa
w condition
nd (South Sh
croclimatic c
prising air
and the grou
surface tha
OP) is calcul
conditions.
d morpholo
on air temp
e and conc
OP calculatio
hological se
quantitative
ults show t
ermafrost di
VALLEY CRO
A)
o Vieira1
de de Lisboa
de Henares
trolled by m
ditions (Wil
now thickn
ne and Harr
energy fluxe
ace and is
ns, thermal
hetlands, Ma
control on
and GST, a
und is evalu
awing and f
ated in ord
gical setting
peratures o
cave locatio
ons show t
tting limits t
e analysis of
hat an exte
istribution.
Págin
ROSS‐SECTIO
mean annu
lliams and S
ness determ
ris, 1994). Ai
es that dete
conditione
l properties
aritime Anta
GST variabi
as well as
ated throug
freezing ind
der to dete
g determine
r by snow
ons reflect
the presen
the depositi
f specific co
ensive netwo
a | 53
ON
al air
Smith,
mines
ir and
rmine
ed by
s and
arctic)
lity, a
snow
gh the
dexes.
rmine
most
cover
snow
ce of
ion of
ntrols
ork of
C
An
The g
in a
(phys
inten
logist
(aka
sedim
samp
In re
logist
patte
Circu
or ev
unto
In th
based
Living
natur
cryoc
and t
distri
the a
COMPARATI
REPRES
ntonio Moli
grain‐sizes d
variety of
sical) techn
nsive, and al
tic implicatio
image‐base
ment size at
pling, in addi
emote areas
tic and con
erned groun
umpolar Acti
ven a destru
uched study
his work, we
d digital ima
gston Island
re and com
clastic depos
thereby pro
ibution by s
areas picture
VE OF PHYS
SENTATIVE
ina 1, Loure
1 Centro de 2 In
3 Uni
distribution i
geomorphi
niques like
lso require
ons. In cont
ed granulom
t a resolutio
ition to othe
s as Antarct
nservation re
nds or spe
ive Layer M
ction of the
ying soils.
e apply sem
ages taken i
ds, South Sh
mposition, r
sits. We obt
oduce a com
sieving and
ed. We expe
SICAL AND
SOILS OF S
nço Bandei
Astrobiología
nstituto Supe
iversidad de A
a.m
s an importa
ic, ecologic
sieving or
direct samp
rast, the opt
metry) are ve
n comparab
er advantage
tica, where
easons, sam
cial interest
onitoring (C
e subject of s
mi‐automate
n a diverse
hetland Arch
ranging fro
ain grain siz
mplete grain‐
sedimentat
ct to evalua
OPTICAL S
SOUTH SHET
ira 2, Pedro
a. INTA‐CSIC.
rior Técnico.
Alcalá. Alcalá
molina@csic
ant paramet
cal and eng
sedimentat
pling with th
tical grain‐si
ery suitable
ble, without
es.
the recollec
mpling is a
t soils that
CALM) sites,
study, mean
ed object de
group of sa
hipelago (An
om tephra
ze measurem
‐size distribu
ion method
te both met
URFICIAL G
TLAND ISLA
o Pina 2, M.A
Torrejón de A
Lisboa, Portu
de Henares,
.es
ter to chara
gineering st
tion are tim
he subseque
ize distribut
methods th
disrupting
ction of sam
key issue. F
t require a
direct samp
nwhile photo
etection alg
mple areas
ntarctica). T
and volcan
ments of the
ution. More
ds with repr
thods for An
RAIN‐SIZE A
ANDS, ANTA
A. de Pablo
Ardoz, Spain
ugal
Spain
cterize the s
tudies. How
me consum
ent terrain
ion analyses
hat can be
the sedimen
mples is res
Furthermore
continuous
pling results
ograph‐base
gorithms to
distributed
These includ
ic ash dep
e individual g
over, we ha
resentative s
ntarctic soils
Págin
ANALYSES
ARCTICA
3, M. Ramo
surficial mat
wever, tradi
ming and la
modificatio
s by photog
used to me
nt body by
stricted owi
e, in the ca
s monitorin
s in a disturb
ed methods
vertical gr
in Deceptio
e soils of di
posits, to c
grains in an i
ave validate
samples tak
s.
a | 54
IN
os 3
terials
tional
abour‐
n and
raphy
easure
direct
ng to
ase of
ng, as
bance
leave
ound‐
n and
iverse
coarse
image
d this
ken in
S
Our
differ
collab
proje
layer
and h
it is
restr
isolat
durin
of sn
Into t
mete
have
net o
the s
varia
heigh
cove
pictu
boreh
const
us to
SNOW DEPO
A
research te
rent sites of
boration, it
ects in the la
r, wich is the
highly mutab
where the
icted. More
tion effect
ng snow me
ow cover ev
the Circump
ers area in D
installed se
of thermo‐sn
surface to in
bility of sno
ht, and assu
r. This data
ures of the C
holes, prov
training the
o understand
OSITION PAT
DECEP
Antonio Mo
1 Centro de 2 Uni
3
eam, condu
f the Antarc
t was supp
ast years. O
e near‐surfac
ble layer is e
majority of
eover, the s
on ground
lting period
volution ent
polar Active
Deception Is
everal temp
now‐meters
nfer snow th
ow cover ba
uming that
can be cros
CALM site. A
ides the inf
extension o
d better the
TTERNS IN R
PTION ISLAN
olina 1, M.A.
Astrobiología
iversidad de A
Universidade
a.m
ucts a long‐
tic Peninsula
orted with
ne of our m
ce layer whic
extremely im
f geomorph
snow cover
temperatur
, are decisiv
ails a better
Layer Monit
sland, locate
erature mon
s (masts wit
hickness) su
ased on the
low variabil
ssed and val
Another net
formation a
of active lay
influence of
RELATION W
ND CALM S
. de Pablo 2
a. INTA‐CSIC.
Alcalá. Alcalá
e de Lisboa. L
molina@csic
‐term resea
a region. In
PERMAPLA
main topics o
ch periodica
mportant bec
hic, hydrolo
r has a cruc
res during t
ves in the ac
r understand
toring (CALM
ed in a plate
nitoring inst
th temperat
pply a comp
e analysis of
lity on temp
idated with
t of temper
about the th
yer. Correlat
f snow cove
WITH ACTIV
SITE, ANTA
, G. Vieira 3
Torrejón de A
de Henares,
isboa, Portug
.es
arch on the
the framew
ANET, ANTA
of interest i
ally freezes a
cause due to
gic, and bio
cial role in
the winter a
ctive layer ev
d of active‐la
M) sites fram
eau at the S
trumentatio
ture sensors
plete record
f the daily t
perature is
the images
ature senso
hermal stat
ion patterns
r into active
VE LAYER E
RCTICA
, M. Ramos
Ardoz, Spain
Spain
gal
e permafros
work of a Spa
ARPERMA Y
s the evolut
and thaws. T
o permafros
ogeochemic
active laye
and the adv
volution. He
ayer dynamic
mework, we
SW of Crate
n. Among t
s at diferent
d of the tem
emperature
a conseque
of a camer
ors at 50 cm
e of the so
s from this in
e layer, and v
Págin
EVOLUTION
s 2
st monitori
anish‐Portug
Y PERMANT
tion of the a
This relativel
st impremea
cal processe
er variability
vection of w
ence, observ
cs.
study a 100
r Lake. Ther
them, a com
t elevations
mporal and s
e stability at
ence of the
ra that takes
m deep in sh
oil at that d
nformation
vice versa.
a | 55
IN
ng in
guese
TAR‐3
active
ly thin
ability,
es are
y. The
water
vation
x 100
re we
mplete
from
spatial
t each
snow
s daily
hallow
depth,
allow
Polyg
seaso
to th
from
conto
imag
Norw
ident
total
polyg
geolo
there
With
new
polyg
surfa
confr
topo
predo
with
tetra
meas
netw
highe
used
Refer
[1] Ma
long‐t
[2] Yo
scienc
CONTRIBU
Maura
gonal terrai
onal process
e formation
ice‐wedges
ours were d
ges (four‐ba
wegian Pola
tified and di
of 6166 po
gon of the 1
ogy, etc.).Ac
e exists a si
the same s
ice‐wedges
gons, which
ace unit. In a
ronted with
graphy is
ominance o
unconsolid
valent verti
sured by m
work). This w
er symmetry
to estimate t
rences:
ackay J.R., 20
terms study.
ong Z., 1995,
ce. Internatio
UTIONS TO Q
NETWORKS
a Lousada 1
1 In2
n patterns
ses of freez
n and growt
s located in
digitized fro
nds RGB+N
r Institute.
gitized into
olygons. Qua
7 networks
ccording to
mple symm
cope [2] pre
that divide
h we tested
addition anc
the density
more rugg
of trivalent v
dated mate
ces (orthog
mean standa
work reinfor
y of the net
he evolutiona
000, Thermal
Geographie P
, Symmetry a
onal Journal o
QUANTIFY T
S. A CASE S
,3, Miguel C
stituto Super2 InstituiçãoCE
3 UNIS, Lo
maura
occur freq
ing and thaw
h of cracks.
the Advent
m the analy
NIR with 0.2
More than
a GIS. Seve
alitative and
(area, perim
[2], no mat
etric relatio
esents a cla
a larger pri
on our ne
cillary param
y led to dete
ged contai
vertices and
erial tend t
gonal), small
ard deviatio
rces that we
work. Addit
ary stage of t
ly induced m
Physique et Q
and other ge
of Solids and S
THE EVOLU
STUDY ON S
Cardoso 2, P
rior Técnico, L
EG / IGOT, Lis
ongyearbyen
a.lousada@is
uently in p
wing cause
The polygo
tdalen valle
ysis of very‐
2 m/pixel o
10,300 ind
enteen large
d quantitativ
meter, lengt
tter how com
on between
ssification s
imary polyg
tworks, by
meters extra
ct clusters o
in network
d an asymm
to contain
ler areas an
on of the le
edge growth
tionally, geo
these networ
ovements in
Quaternaire, V
eometric con
Structures, Vo
UTIONARY S
SVALBARD
Pedro Pina 1
Lisboa, Portu
sboa, Portuga
n, Norway.
t.utl.pt
periglacial re
the soil to e
onal network
ey, Svalbard
‐high spatial
of spatial re
ividual poly
st of these
ve paramet
h, type of th
mplex a surf
the numbe
scheme base
on into sma
computing
acted from t
of networks
ks with lar
metric geom
networks
d larger sym
ength of th
h leads to p
ometric and
ks.
ice‐wedge po
Vol. 54, pp. 41
nstraints of s
ol.32, No. 2, p
TAGE OF P
NETWORKS
1, Gonçalo V
gal,
al,
egions of t
expand and
ks studied in
archipelago
resolution
esolution),
ygons in 120
networks w
ers were ex
he vertex (tr
face networ
ers of vertice
ed upon the
aller seconda
the density
the DTM, su
. For instanc
rger polygo
metry. In con
with larger
mmetry (bein
he polygons
polygon sub
topological
olygons, wes
‐68.
urface netwo
pp. 173‐201.
Págin
POLYGONAL
S
Vieira 2
the Earth, w
contract, le
n this work
o, at 78º N.
remotely se
acquired b
0 networks
were analyse
xtracted for
ri or tetrava
rk appears t
es and poly
e developme
ary (and ter
y of polygo
uch as slope
ce, regions w
ons, perce
ntrast, flat z
r percentag
ng the symm
s faces for
bdivision and
features m
stern arctic co
orks in natur
a | 56
where
eading
result
Their
ensed
y the
were
ed in a
r each
alent),
to be,
ygons.
ent of
rtiary)
ns by
e that
where
ntage
zones
ge of
metry
each
d to a
may be
oast: a
re and
SEDI
Ale
3 Dep
Serra
Centr
types
durin
Serra
Portu
ident
types
betw
Howe
befor
Our
analy
analy
sedim
matr
analy
sectio
This
with
thin‐s
interp
of qu
Our
signif
envir
Quat
RECON
IMENTOLOG
xandre Nie
1 Ce
partment of G
4 Departam
a da Estrela
ral Cordillera
s of granito
ng the Last
a da Estrela
ugal. Vieira
tifying sever
s of debris‐f
ween glacial
ever, a deta
re and abso
work is bas
ysis and dat
ysis using G
mentary unit
ix elements
ysed for gra
on micromo
poster pres
other techn
section micr
pretation of
uartz grains t
goals are
ficance of t
ronment pr
ternary evolu
NSTRUCTING
GICAL ANAL
euwendam1
entro de Estud2 Departame
Geomorpholo
mento de Geo
is the highe
a. The moun
oids and me
Glacial Max
a is a landm
(2004) pro
ral slope dep
flow deposit
l and perig
ailed and sys
lute ages are
sed on the
ting, suppo
GIS. The se
ts and struc
s. Samples f
ain‐size analy
orphology an
ent results
niques, aids
romorpholo
f componen
to analyse fr
to contrib
the differen
ocesses an
ution of the
G COLD CLIM
LYSIS OF SL
, Carlos Sch
Go
dos Geográfic
ento de solos,
ogy, Faculty of
logia, Faculda
alexan
est mountai
ntain has a s
tasediments
ximum and
mark in stu
oduced a d
posit types a
ts. Based on
glacial evide
stematically
e also lackin
systematica
orted by de
edimentolog
ctures, fabric
from differe
ysis of coars
nd exoscopy
from key sl
in the inter
ogy, concern
nts, features
rost‐weathe
ute to the
t types of s
d also to d
slope enviro
MATE PALE
LOPE DEPOS
haefer2, Ba
onçalo Viei
cos‐IGOT, Un
, Universidad
f Geography
Poland.
ade de Ciênci
ndretn@gma
in in Portug
strong relief
s. Most of t
its morphol
udies of gla
detailed geo
and outcrop
n the geomo
ence, a firs
y sedimonto
ng.
ally applicat
tailed geom
gical analysi
c analysis, c
ent stratigra
se and fine
y of quartz g
ope deposit
rpretation of
ning the mic
s and fabrics
ering microst
e better un
slope depos
develop a
onment of t
EOENVIRON
SITS (SERRA
rbara Woro
ra1
iversidade de
e Federal de
and Regional
a da Universi
ail.com
gal (1993 m A
f and a litho
the western
logy is dom
acial and pe
omorpholog
ps of stratifi
orphological
st relative
logical analy
tion of sed
morphologic
s includes
last morpho
aphic units
fractions, o
grains.
ts: a) clast f
f colluvial de
croscopic id
s in soils and
tructures.
nderstandin
sits includin
chronologic
he mountain
MENTS FRO
A DA ESTRE
onko3, Conc
e Lisboa, Port
Viçosa, Brasil
l Studies, Univ
dade de Lisbo
ASL) and pa
ological dive
n plateau ar
minated by g
eriglacial ge
gical map o
ed slope, he
analysis of
chronology
ysis has not
imentologic
cal surveying
macroscopi
ometry and
of slope de
organic matt
fabric analys
epositional e
entification,
d sediments
g of the
g clarifying
cal framewo
ns of Weste
Págin
OM THE
ELA,PORTU
ceição Freit
tugal
l
versity of Wa
oa, Portugal
art of the Ib
ersity with se
rea was glac
glacial landf
eomorpholo
of the mou
ead and diff
the relation
was prese
t been cond
cal techniqu
g and by s
ic descriptio
characterist
eposits are
ter content,
sis, that tog
environmen
, descriptio
s and c) exo
morphogen
the role of
ork for the
rn Iberia.
a | 57
UGAL)
tas4,
arsaw,
berian
everal
ciated
forms.
ogy in
ntain,
ferent
nships
ented.
ucted
ues of
spatial
on of
tics of
being
, thin‐
gether
nts; b)
n and
scopy
netical
f cold
Late
The o
the o
activa
mast
Anta
seen
abstr
whal
Anta
storie
Anta
Deep
talke
smell
plung
start
Keyw
IN AND BE
objective of
oral‐visual na
ated when
ter plot of th
rctic experie
as human‐l
ract art, the
ebones are
rctica is the
es of its fir
rctic tourism
pest affectua
d about the
ls of pengui
ge, thick mo
to cry.
words: Antar
EYOND THE
this study w
arratives of t
touring in A
he Antarctic
ence rotates
like creature
e glaciers ar
enchanting
only land th
rst explorer
m presents
al encounte
e powerful s
ins and seal
orning mist,
rctic tourism
E VISUAL GA
ANTAR
D
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tung
was to unw
tourists in o
Antarctica.
c tourism im
s around th
es, the iceb
re moving a
g artifacts, m
hat has no m
rs. In contra
an exampl
rs of tourist
sounds of c
colonies, th
which conce
m, imaginary,
AZE OF THE
RCTIC WILD
Dennis Zue
ES‐ISCTE (Lisb
gus66@gmail
rap the Ant
order to und
What are t
maginary? Mo
e theme of
ergs are sp
and living re
memories o
myths of orig
ast to the
le of multis
ts come from
calving glaci
he caresses
ealed the lan
, Zodiac, enc
E TOURISTS
ERNESS
v
bon)
l.com
arctic touris
erstand whi
he key elem
ost of the vi
“humanized
oken about
eminders of
of once pro
gin but comp
“gaze” cen
sensuous, n
m engaging
ers and me
of Antarcti
nd and upon
chantment
: ENCHANT
sm imaginar
ch other sen
ments comp
sualization o
d nature”:
as the perf
the power
olific whale‐h
pensates th
tered appro
on‐ocularce
various sen
ditating bra
c wind, and
n seeing wh
Págin
TMENTS OF
ry and go be
nses and ho
prising the g
of Antarctic
the penguin
rfect examp
of nature,
hunting ind
is with the h
oach to tou
entric geogr
ses: intervie
ash ice, the
d refreshing
ich people w
a | 58
eyond
ow are
grand
ca and
ns are
les of
while
ustry.
heroic
urism,
raphy.
ewees
awful
Polar
would
PO
P
Jo
1 I
One
emer
scien
Polar
provi
relate
was m
proje
Viva,
Caree
Inter
with
proje
an e
teach
Cidad
ORTUGAL
PROJECTS “
osé C. Xavie
nstitute of M2 B
3 Universi
of the main
rgent polar
nce, educatio
r scientists
ided an exc
ed discipline
mostly carri
ects “Profes
and endors
er Scientist
rnational (PE
schools, un
ect aims to p
educational
hes/educato
dania). Thes
EDUCATI
PROFESSIO
BRINGIN
er 1,2, P. Azi
Fer
Marine Resear
British Antarct
ty of Lisbon, 4
5 Instituto
reasons wh
nation dur
on and outr
to schools
cellent route
es). After ou
ed out by in
ssion: Polar
sed by the Po
ts (APECS P
EI). The first
nder POLAR
provide tool
pamphlet,
ors and an
e projects st
ON AND O
ON: POLAR S
NG POLAR S
nhaga1, S. L
rreira5, V. Pe
ch (IMAR‐CM
tic Survey, Hi
Faculty of Sci
CEG‐IGOT, Un
o de Educaçã
JC
hy Portugal w
ring the Int
reach output
s, engaging
e to engage
ur education
ndividual inst
Scientist” a
ortuguese P
Portugal an
t projects a
R WEEKS o
ls and mater
educationa
exhibition (
tarted officia
OUTREAC
SCIENTIST”
SCIENCE TO
Lourenço3,
ereira1 and
MA), Universit
gh Cross Mad
iences, Camp
niversity of Li
o e cidadania
was highligh
ternational
ts. Bringing
teachers/e
e the young
nal program
titutions. W
and “Educat
Polar Progra
nd APECS i
aims to reinf
rganized by
rials to scho
al films, ed
(in coopera
ally in 2013 a
CH: OUR N
” AND “EDU
WIDER AU
G. Vieira4,
J. C. Marqu
y of Coimbra,
dingley Road,
po Grande, 174
isbon, Portug
a, Mamarrosa
net
hted as a su
Polar Year
the researc
educators a
ger generati
m, LATITUDE
e wish to int
tion PROPO
m PROPOLA
internationa
force the lin
y APECS an
ools on pola
ducational
tion with t
and the first
EW EDUCAT
UCATION PR
UDIENCES
A. S. David
ues1
, 3001‐401 Co
, Cambridge,
49‐016 Lisbon
gal
, Portugal
ccessful exa
2007‐2008,
ch carried ou
nd scientist
ons to scien
60!, educati
troduce the
OLAR”, supp
AR, Associat
al) and by
nks between
nd PEI, whe
r science. Th
materials, a
he Instituto
results will
Págin
TIONAL PO
ROPOLAR
d4, B. Cruz1,
imbra, Portug
UK
n, Portugal
ample of a r
was throug
ut by Portug
ts together
nce (and sc
ion and out
e new educa
ported by C
tion of Polar
Polar Educ
n polar scie
ereas the se
hese may in
a workshop
o de Educaç
be presente
a | 59
LAR
R”
S.
gal
recent
gh its
guese
r, has
cience
treach
tional
iência
r Early
cators
entists
econd
nclude
p for
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NOTAS
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