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ANNALES HISTORICO-NATURALES MUSEI NATIONALIS HUNGARICI Tomus 66. Budapest 1974. Trochiscia (Chlorophyta) Red Snow from Swedish Lapland By E. KOL , Budapest Abstract Trochiscia red snow is a rare kryoseston discoloration. Until now the mass occurrence of Trochiscia americana KOL in North America and that of Trochiscia rubra Kol in Norway were found to cause red snow. In the snow-field of Swedish Lapland Trochiscia americana var. lapponica var. n. caused red snow. 24 figures. Red snow is the most frequent kryoseston discoloration. It is a well known natural phenomenon in the higher mountains of both the northern and the southern hemisphere and even in the Antarctic. Instances, however, when two red snows are caused by one -and the same algal species, or identical assemblies of microorganisms are seldom found. From scientific view, therefore, it is of great impotance to collect samples from each red snow, because generally in each occasion a new algal species or a new assembly of algae is found in them. In this paper too, an entirelly new Trochiscia red snow found in the Swedisn Lappland will be reported on. Red snow is a frequent natural phenomenon in the Scandinavian mountains. The snow vegetation of Norway has been dealt with by a number of authors: BOHLIN (1893, 1895), BOLDT (1888), BORGE (1899), LAGERHEIM (1883, 1894), NORDSTEBT (1978), SKUJA (1964, STRÖM (1923, 1926), WILLE (1879, 1903), WITTROCK (1883), KOL (1968). Red snow caused by immense masses of C'hlamydomonas nivalis (BAU .) WILLE ( KOL 1968) has become known from numerous points in Norway. KOL (1963: 156) reports on three cases of red kryoseston discoloration from the vicinity of Finse, Norway which were caused by the mass occurrence of various micro- organisms. The red snow of Hardangerj ökelen was caused almost without exception by Ghlamydomonas nivalis (BAU .) , WILLE , tough Scotiella nivalis (SHUTTLEW .) FRITSCH and in a negligible quantity other microorganisms also occurred there. In the rose-colou- red snow of the other snow-field Trochiscia rubra KOL ( = Trochiscia cryophila var. rubra KOL ) dominated, and besides this species Chlamydomonas nivalis (BAU.) WILLE and also other microorganisms played an important role. In the red snow of the third snow-field approximately 85 percent of the microorganisms was represented by G hlamy- domonas sanguinea LAGERH. Collection — Norddalsfjeld Mt. over Ketterjaure Lake, Swedish Lappland, north latitude 68,5 N, circa 750 m, brick-red snow, circa on 3 m 2 surface. 10. August 1973 leg. A. BERCZIK . Also here I wish to express my best thanks to Dr. A. BERCZIK for the most valuable snow sample collected for me. Microorganisms in Trochiscia americana var. lapponica var. n. red snow The bulk of the brick-red snow collected in Norddalsfjeld mountains of Swe-, dish Lappland consisted of Trochiscia americana var. lapponica var. n. (Figs. 2—9). Table shows that in the red snow eight algae and two kryofungus species were living. From among the algal species five were kryobionts and two kryoxens: Gloeocapsa ralfsii (BOHL.) LEMM . and Stigonema sp.

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A N N A L E S H I S T O R I C O - N A T U R A L E S M U S E I N A T I O N A L I S H U N G A R I C I T o m u s 66. Budapest 1974.

Trochiscia (Chlorophyta) Red Snow from Swedish Lapland

B y E . K O L , Budapest

Abstract — Trochiscia red snow is a rare kryoseston discoloration. U n t i l now the mass occurrence of Trochiscia americana K O L i n N o r t h America and that of Trochiscia rubra K o l i n Norway were found to cause red snow. I n the snow-field of Swedish Lapland Trochiscia americana var. lapponica var. n . caused red snow. — 2 4 figures.

Red snow is the most frequent kryoseston discoloration. I t is a well known natural phenomenon i n the higher mountains of both the northern and the southern hemisphere and even i n the Antarct ic . Instances, however, when two red snows are caused by one -and the same algal species, or identical assemblies of microorganisms are seldom found. From scientific view, therefore, i t is of great impotance to collect samples from each red snow, because generally i n each occasion a new algal species or a new assembly of algae is found in them. I n this paper too, an entirelly new Trochiscia red snow found i n the Swedisn Lappland w i l l be reported on.

Red snow is a frequent natural phenomenon in the Scandinavian mountains. The snow vegetation of Norway has been dealt w i t h by a number of authors: B O H L I N ( 1 8 9 3 , 1 8 9 5 ) , B O L D T ( 1 8 8 8 ) , B O R G E ( 1 8 9 9 ) , L A G E R H E I M ( 1 8 8 3 , 1 8 9 4 ) , N O R D S T E B T ( 1 9 7 8 ) , S K U J A ( 1 9 6 4 , S T R Ö M ( 1 9 2 3 , 1 9 2 6 ) , W I L L E ( 1 8 7 9 , 1 9 0 3 ) , W I T T R O C K ( 1 8 8 3 ) , K O L ( 1 9 6 8 ) . Red snow caused by immense masses of C'hlamydomonas nivalis ( B A U . ) W I L L E ( K O L 1 9 6 8 ) has become known from numerous points in Norway.

K O L ( 1 9 6 3 : 1 5 6 ) reports on three cases of red kryoseston discoloration from the v ic in i ty of Finse, Norway which were caused by the mass occurrence of various micro­organisms. The red snow of Hardangerj ökelen was caused almost wi thout exception by G hlamydomonas nivalis ( B A U . ) , W I L L E , tough Scotiella nivalis ( S H U T T L E W . ) F R I T S C H and in a negligible quant i ty other microorganisms also occurred there. I n the rose-colou­red snow of the other snow-field Trochiscia rubra K O L ( = Trochiscia cryophila var. rubra K O L ) dominated, and besides this species Chlamydomonas nivalis ( B A U . ) W I L L E and also other microorganisms played an important role. I n the red snow of the t h i r d snow-field approximately 8 5 percent of the microorganisms was represented by G hlamy­domonas sanguinea L A G E R H .

C o l l e c t i o n — Norddalsfjeld M t . over Ketterjaure Lake, Swedish Lappland, n o r t h lat i tude 6 8 , 5 N , circa 7 5 0 m , brick-red snow, circa on 3 m 2 surface. 1 0 . August 1 9 7 3 leg. A . B E R C Z I K . Also here I wish to express m y best thanks to Dr . A . B E R C Z I K for the most valuable snow sample collected for me.

Microorganisms i n Trochiscia americana var . lapponica var . n . red snow

The b u l k o f the b r ick- red snow collected i n Norddalsf je ld mounta ins o f Swe-, d i sh L a p p l a n d consisted o f Trochiscia americana var . lapponica var . n . (Figs. 2—9). Tab le shows tha t i n the red snow eight algae and t w o kryofungus species were l i v i n g . F r o m among the algal species f ive were k r y o b i o n t s and t w o k r y o x e n s : Gloeocapsa ralfsii ( B O H L . ) L E M M . and Stigonema sp.

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Fig . 1. Glúamydomonas sanguinea L A G E R H . w i t h gelatinous sheath (x 500). Figs. 2 — 10. Trochiscia americana var. lapponica var. n . (x 1000) : 2 = older cell w i t h smooth cell-wall, 3 = cell w i t h irregularly thickened wal l , 4 '— cell w i t h warted cell-wall, 5 = cell-division, the wal l of the mother cell is gelatinized, 6 = cell-division, 7 = very young daughter cell,

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9 0 percent o f the red snow vegetat ion was represented b y Trochiscia americana v a r . lapponica var . n . , and 1 0 per cent o f i t b y Chlamydomonas sanguinea L A G E R H . {Figs . 1, 1 5 , 16 , 2 4 ) , Cryocystis granulosa K O L (Figs. 1 1 — 1 3 ) , Scotiella norvegica K O L F i g . 1 7 ) , Scotiella nivalis ( S H U T T L E W . ) F R I T S C H . (Figs. 2 1 — 2 3 ) , Gloeocapsa ralfsii ( B O H L . ) L E M M . (F ig . 2 0 ) , Stigonema sp., Chionaster bicornis K O L (F ig . 18),C'Monaster nivalis ( B O H L . ) W I L L E (F ig . 1 9 ) . Besides microorganisms there were also fragments of p lan t o r ig in and fungus spores present i n the snow sample. I t is an interes t ing feature o f kryoseston discolorat ion tha t black snow is ming led to the b r i ck - red snow.

Comparative data of the microorganisms found in the red snow

Nordda l s f j e l d E n v i r o n s M i c r o o r g a n i s m M t . Swedish of F inse

L a p p l a n d N o r w a y

A l g a e Chlorophytae

Chlamydomonas nivalis ( B A U . ) W I L L E + + G hlamydomonas sanguinea L A G E R H . + + Cryocystis (Chodatella) granulosa K O L + Mesotaenium berggrenii ( W I T T R . ) L A G E R H . + Scotiella nivalis ( S H U T T L E W . ) F R I T S C H + + Scotiella norvegica K O L + Raphidonema nivale L A G E R H . + + Trochiscia americana var. lapponica var. n. + Trochiscia rubra K O L + {Trochiscia cryophila var. rubra K O L )

Cyanophyta Cloeocapsa ralfsii ( H A R V . ) L E M M . + Stigonema sp. +

F u n g i Chionaster bicornis K O L + + Chionaster nivalis ( B O H L . ) W I L L E + + Chytridium chlamydococcii A . B R . +

Table shows t h a t i n the b r ick- red snow o f Swedish L a p p l a n d m a n y such microorganisms occurred t h a t were also found i n the red snow i n the environs o f Finse ( K O L 1 9 6 3 ) . Trochiscia species seldom occur i n such quant i t ies t h a t w o u l d cause discolorat ion of snow. I n the l i t e ra ture , there is men t ion made, t o m y k n o w ­ledge, on ly o f t w o cases of Trochiscia kryoseston discolorat ion. I n more t h a n one snow-f ie ld o f the R o c k y Mounta ins , N o r t h Amer ica , the Trochiscia americana ( K O L 1 9 6 8 ) , and i n the snow-fields at Finse, N o r w a y the Trochiscia rubra K O L ( K O L 1 9 6 3 , 1 9 6 8 ) caused red snow.

8 = greater daughter cell w i t h t h i n cell-wall, 9 = cell w i t h cell-wall decorated w i t h small spines and warts, 1 0 = cell w i t h spined cell-wall. Figs. 1 1 — 1 3 . Cryocystis granulosa K O L (x 1 0 0 0 ) in different stages of development. — Fig . 1 4 . Chionaster nivalis ( B O H L I N ) W I L L E — Figs. 1 5 — 1 6 , 2 4 . Chlamydomonas sanguinea L A G E R H . ( X 5 0 0 ) ; various resting stages: 1 4 = w i t h layered cell-wall, 1 5 = w i t h th ick cell-wall, 2 4 = w i t h gelatinous sheath. — Fig. 1 7 . Scotiella norvegica K O L ( X 1 0 0 0 ) . — Fig. 1 8 . Chionaster bicornis K O L ( X 1 0 0 0 ) . — Fig. 1 9 . Chionaster nivalis ( B O H L . ) W I L L E ( X 1 0 0 0 ) . -* F ig . 2 0 . Cloeocapsa ralfsii

( B O H L . ) L E M M . ( X 1 0 0 0 ) . — Figs. 2 1 — 2 3 . Scotiella novalis ( S H U T T L E W . ) F R I T S C H . ( X 1 0 0 0 ) i n different stages of development.

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62 E . K O L

The Trochiscia red snow reported here is the t h i r d one the alga o f w h i c h is k n o w n . I t follows f rom the aboves t ha t the three red snows were caused b y different Trochiscia species each. I t is characteristic, tha t near ly every algal species found i n the snow samples was i n an early stage o f development, and on ly a few comple­t e l y developed forms and small numbers o f species i n the rest ing stage occurred.

Chlamydomonas sanguinea L A G E R H . (Figs. 1, 15, 16, 24)

Spherical, b r igh t - red cells, 32—40 p i n diameter, w i t h t h i n (F ig . 1) or t h i c k layered cel l -wal l (Figs. 15—16) occasionally w i t h gelatinous sheath (F ig . 24). O n l y a few nonmot i l e forms were found.

The species was described f i r s t b y L A G E R H E I M f rom the red snow of P ich incha volcano, South Amer ica . Since then i t has been found i n more t h a n one places i n Europe. I t was found to cauese red snow i n the Alps ( K O L 1968), i n the H i g h T a t r a ( K O L 1969), and near Finse, N o r w a y ( K O L 1963). I t is one o f the rare k r y o b i o n t i c algal species t h a t cause kryoseston discolorat ion i n b o t h the southern and the n o r t h ­ern hemisphere.

Cryocystis granulosa K O L Figs. 11—13) (= Chodatella granulosa K O L )

Ova l or ovo id cells, 10—15 /j, wide and 15—27 p long, w i t h cel l -wal l orna­mented w i t h war ts , were found i n various stages o f development i n the snow sample. The species is abundant i n the N o r t h Amer i can R o c k y Mounta ins and i n the snow-f led o f Grönland.

Scotiella nivalis ( S H U T T L E W ) F R I T S C H (Figs. 21—23)

One of the most frequent k r y o b i o n t s is bipolar . I t is ve ry frequent i n the snow-fields o f b o t h the n o r t h e r n and the southern hemisphere.

The specimens o f each species found i n the snow sample o r ig ina t ing f rom Swedish L a p p l a n d were i n var ious stages o f development . The spherical young and ova l cells had various sizes and were numerous. There were on ly a few ind iv idua l s w i t h cel l -wal l ornamented w i t h r ibs.

Scotiella norvegica K O L (F ig . 17)

Spindle shaped cells, 15 /j, wide b y 40 p long, w i t h sp i ra l ly decurrent r ibs . I n the sample on ly a few specimen were found . This algal species was f i r s t described b y K O L (1968) f rom the red snow near Finse.

Trochiscia americana var . lapplandica var . n . (Figs. 2—10)

P r o x i m u m adest ad Trochiscia americana K O L sed dif fer t ab eo: 1. coloris ce l lu larum, 2. o rnamenta t ion ce l lu larum, 3. dimensione ce l lu larum.

H a b i t , i n n iv ibus rubr i s Swedish L a p l a n d .

D e s c r i p t i o n — Spherical cells, 10—20 p i n diameter. The cell-walls o f the young cells are t h i n and smooth (Figs. 2, 7, 8), those o f the older ones become th ickened (F ig . 2), f i r s t undu la ted (F ig . 3) later decorated w i t h small , sparsely loca-

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t ed war ts f i n a l l y w i t h spines. The t h i c k , older cel l -wal l is b rownish (Figs. 4 , 9 R

1 0 ) . The cells conta in m u c h rose-coloured o i l , ha rd ly any starch. Py reno id was no t visible i n the cells.

Reproduc t ion takes place b y autospore fo rma t ion . The daughter i nd iv idua l s w i t h t h i n , smooth cel l -wal l escape b y means of the gela t in iza t ion o f the cel l -wall o f the mother cell (Figs. 5 , 6 ) . This microorganism bears resemblance most t o the Trochiscia americana K O L species. I t differs f rom i t , however, on the basis o f the fo l lowing features: 1. the cell is l igh t br ick- red . 2 . the w a l l o f the cell is ornamented w i t h war ts . 3. i t is smaller.

K O L ( 1 9 6 8 ) found the Trochiscia americana K O L species to occur i n several places o f the N o r t h Amer i can R o c k y Mounta ins , f rom where she had described i t f i rs t .

References

B O H L I N , K . (1893): Snöalger fram Pite Lappmark. - Bot. Notiser, p. 42 - 46. B O H L I N , K . (1895): Über Schneealgen aus Pite Lappmark. - Bot. Gbl., 64: 4 2 - 4 5 . B O L D T , R . (1888): Om förekomsten af röd snö i finska Lappmarken. — Bot. Notiser., p.

233-234 . B O R G E , O. (1911): Die Süsswasseralgenflora Spitzbergens. — Videnskaps. Skr. I . Nath.,.

Naturw. KI., 110 5 - 39. K O L , E . (1957): Über die Verbreitung der schnee- und eisbewohnenden Mikroorganismen

i n Europe I . — Arch. f. Hydrobiol., 52: 574 — 582. K O L , E . (1963) : On the red snow of Finse (Norway). — Ann. Hist.-nat. Mus. Nat. Hung.T

55: 155-160. K O L , E . (1968): Kryobiologie und Limnologie des Schnees und Eises, I . Kryovegetation.

— Die Binnengewässer, 24: 1—216. K O L , E . (1969): Chlamydomonas sanguinea Lagerh. in the H i g h Tatra. — Ann. Hist.-nat

Mus. Nat. Hung., 61 : 141 - 145. L A G E R H E I M , G. (1883): Bidrag t i l l kännedom on snöfloran i Lules Lappmark. — Bot-

Notiser, p . 230-235 . S K U J A , H . (1964): Grundzüge der Algenflora und Algen vegetation der Fjeldgegend u m

Abisko i n Schwedisch Lappland. — Nova Acta Regiae Soc. Sc. Upsaliensis, Ser. I V . , 18: 1-465.

S R T Ö M , M . K . (1923): Snow Algae from the Sarek Mountains. — Naturw. Unters, d. Sarek-geb., 35: 522-524 .

S R T Ö H , M . K . (1926): Norwegian Mountains Algae. - Skr. Norske Vid. Akad. p . 1 - 2 6 3 . W I L L E , N . (1903): Algologische Notizen I X — X I V . — Nyt magazin for Naturvidenskab.,

4 1 : 8 8 - 1 8 9 . W I T T R O C K , V . B . (1883) : On snöns och isens flora särskildt i de arktiska trakterna. — A .

E . N O R D E N S K I Ö L D : Studier och forsk. föranledda af mina resor i Höga Norden., p . 65 — 124.

Author's address: Dr. E. K O L Botanical Department of the Hungarian Natural History Museum H—1146 Budapest, Vajdahuny ad vár Hungary

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