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Systematic Relationships among Birds
• Hypotheses for the evolution of birds
• Determines how your bird guide is arranged
• Contentious– Morphology
• What to measure, convergent evolution
– Fossils• Missing links / sample bias• Lack of soft parts
– DNA• How to calibrate• Which and how many genes to use• What species to include in analysis
(outgroups especially)
Mayr 2014
Fundamental Divisions
• Paleognathae– Primitive palate
(left image shows better than Fig 3.6 in text)
– Monophyly of many flightless birds
• Hoatzin primitive but not basal to Neognathae – Opisthocomidae
in clade 6– Galloanserae is
basal and monphyletic
In Rheas, Tinamous, Ostrich, Cassowaries, Emu, Kiwi, and extinct Moas and Elephant Birds the vomar bone extends back to articulate with palatines and pterygoids to separate both from the parashenoid rostrum
Tertiary Big Bang?
(Feduccia 2003)
K-T boundary (end of Cretaceous; 65 my) Volcanism, mountain building, regression of continental seas meteor in Mexico (Chicxulub crater in Yucatan) Dinosaur extinctions
Theory in accordance with Fossil record
But Birds were Evolving in Southern Hemisphere
• Gondwanaland
(Cracraft 2001)
DNA studies suggest modern birds radiated before KT boundary
Vegetation of Antarctic area was not greatly affected by impact
Ancestor of Passeriformes was Gondwanan; divergence began before KT
• Acanthisitta = New Zealand Wrens are most primitive passerine and sister to Suboscines and Oscines (songbirds)
• They diverged from other passerines about 82my, ancestors moved across connected Antarctic
• Oscine and Suboscine songbirds began to diverge about 77my
(Barker et al. 2004)
(Ericson 2008, Ericson et al. 2006)Ratites and Tinamous
Nightjars, owlet-nightjars, potooes, oilbird, frogmouths, hummingbirds, swifts
Shorebirds, gulls, auks
Pelicans, cormorants, herons, storks, cranes, rails, loons, penguins, albatrosses, cuckoos, turacos, bustards
Parrots and Passerines
Accipitrid diurnal raptors, osprey and secretarybird, rollers, woodpeckers, trogons, mousebirds, owls
Pheasants, quails, currasows, ducks, geese, swans
Heterogeneous assemblage of enigmas
177 mya
67 mya
68 mya
63 mya
75 mya
95 mya
More Substantial Divergence Was Even Earlier
(Ericson et al. 2002)
(Cracraft 2001)
So, the Real Explosion was After the KT event
(Barker et al. 2004)
Red = AustralasiaGreen = Africa and EurasiaBlue = North and South AmericaGrey = ambiguous ancestral / current area
(Barker et al. 2004)
Mayr 2014
Ravens
During the last several million years land connections (via Beringia) between New and Old Worlds waxed and waned with glaciation. Beringia was dry and offered land passage.
50ka
Corvids Invade Our World
Tied to changes in vegetation and sea levelTertiary forests of Australia were being
replaced by deserts perhaps forcing corvid ancestors (related to Birds of Paradise and Orioles) to leave Australia and head north in Oligocene and Miocene to Asia, following northward movement of tropical forests
6-8 mya in MioceneNew World Jay ancestor from forests of
southeast Asia, radiate in South America (first) and North America
15,000 ya – 2 mya in PleistoceneOld World Jay (Gray Jay)NutcrackerMagpieCrowRaven
(from article on evolution of cats; Johnson et al. 2006; Science 311:73-77)
Ravens
• 4 clades diverging in Africa 1.7-3.8my
• Corvus corax ancestor diverges (closest relative is C. albus) shortly thereafter
• C. corax invades New World 2my and new and old world ravens begin independent evolution
– Old world raven spins off Canary Island Raven 650,000 yr
– New world ravens spins off Chihuahuan Raven
• C. corax reinvades New World 15,000 years ago
Complexity Revealed By Genetic Analyses
• Common Raven– ~15,000 years ago old
world ravens again invaded the new world via Beringia
• Holarctic and California clade of ravens now found in North America, but they are becoming more similar, not diverging as they had in past.
– Giving us new insights into what constitutes a “species”
Fig. 1. FROM DELANEY et al. 2008---Distribution of Island and Western scrub-jays, with associated geographic trends in morphological characteristics. Species distributions are adapted from Curry et al. (2002); orange = Aphelocoma insularis, green = Californica group of Aphelocoma californica, light blue = Woodhouseii group of Aphelocoma californica, and dark blue = sumichrasti group of Aphelocoma californica.
Florida Scrub-jay
Scrub-jays
Currently we recognize 3 species, but there are most likely 5 and maybe 6
isolation has been of paramount importance and novel selective pressures from foods eaten (oaks versus other seeds)
A. un. griscomi
A. un. unicolor
A. un. oaxacae
A. un. concolor
A. un. guerrerensis
CITATION: McCormack, Peterson, Delaney, Knowles, in prep.
Unicolor Jay (Aphelocoma unicolor)
• The 7 Aphelocoma ultramarina traditional subspecies are given in abbreviations (A. ul. Xxx) on the map, the colors refer to the 4 groups I refer to in the text now. These could be labeled as the Central group (orange), the Eastern group (yellow), the Ultramarina group (blue), and the Wollweberi group (green). The four groups are from McCormack et al. 2008.
• McCormack, J. E., Peterson, A. T., Bonaccorso, E., and T. B. Smith. 2008. Speciation in the highlands of Mexico: genetic and phenotypic divergence in the Mexican jay (Aphelocoma ultramarina). Molecular Ecology 17:2505-2521.
A. ul. arizonae
A. ul. wollweberi
A. ul. gracilis
A. ul. colimae A. ul. ultramarina
A. ul. potosina
A. ul. couchii
Mexican Jay
• Rapid diversification of the 3 major clades
• Deep divergence in A. unicolor
• Major phylogenetic structure in Mexican jays
• Florida scrub-jays basal within scrub-jay complex
McCormack, Peterson, Delaney, Knowles, in prep.Also could cite: Delaney et al. 2008, Auk (for scrub jays)McCormack, Peterson, Bonaccorso, and Smith 2008, Mol Ecol (for Mexican jays)
Timing of diversification in Aphelocoma
Diversification much older than previously thought– Major lineages diverging quickly in the
late Miocene– Transvolcanic Mexican jay ancient lineage– Few divergence events in the major
glacial period (<0.7 mya)
McCormack, Peterson, Delaney, Knowles, in prep.
• Major division N and S of the Isthmus (6% div)
• Pliocene• Divergences north of
Isthmus potentially linked to glacial cycles– Time frame correct for
when Mexico was influenced by glacial activity further north
3.5 (6.0,2.5)
2.8 (3.9,1.3)
0.9 (2.0,0.5)
0.5 (1.2,0.3)
, Guatemala
Honduras
A. un. griscomiA. un. unicolor
A. un. oaxacae
A. un. concolor
A. un. guerrerensis
McCormack, Peterson, Delaney, Knowles, in prep.
Unicolor Jay
4.6 (7.4,3.7)
2.8 (3.7,1.5)
1.8 (2.4,0.9)
• Genetic variation is not continuous & no haplotype sharing among clades
• Transvolcanic Mexican jays have a long and independent history
• New major clade in the rugged mountains of the Central Plateau
• Pleistocene glacial cycles likely not the cause of major diversification events (diversification preceeded the effect of glacial cycles in Mexico which were 650000 yr)
• West group very structured– North to south (food
diffs)– East/West division in
sky islands (10,000yr isolation by dispersal barriers)
McCormack, Peterson, Bonaccorso, & Smith Mol Ecol 2008
A. ul. arizonae
A. ul. wollweberi
A. ul. gracilis
A. ul. colimae A. ul. ultramarina
A. ul. potosina
A. ul. couchii
Conservation Implications
• Widespread, common species may actually be comprised of many, relatively rare and specialized species
• Areas on the fringes of a “species” distribution and therefore perhaps not all that important might be in the core of revised “species” and therefore of high significance to biodiversity– Mexican Highlands are one such area
with potentially many endemic species that we currently fail to recognize
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