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Lichens, Bryophytes and Terrestrial Algae of the Lake Untersee Oasis (Wohlthat Massiv, Dronning Maud Land, Antarctica)

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Lichens, Bryophytes and Terrestrial Algae of the Lake Untersee Oasis (Wohlthat Massiv, Dronning Maud Land, Antarctica) CZECH POLAR REPORTS 10 (2): 203-225, 2020 Lichens, bryophytes and terrestrial algae of the Lake Untersee Oasis (Wohlthat Massiv, Dronning Maud Land, Antarctica) Mikhail Andreev1*, Dale Andersen2, Lyubov Kurbatova1, Svetlana Smirnova1, Olga Chaplygina1 1Komarov Botanical Institute of the Russian Academy of Sciences, Professor Popov St. 2, 197376 St. Petersburg, Russia 2Carl Sagan Center, SETI Institute, 189 Bernardo Ave., Suite 100, Mountain View, California 94043, USA Abstract Lake Untersee is the largest ice-covered freshwater lake in the interior of East Antarctica. The mountain oasis is situated around it in the Gruber Mts. of the Wohlthat Massif. For approximately 7,000 years the area has been free of ice and the local climate relatively stable. It is very severe, cold, and windy and dominated by intense evaporation and sublimation but with little melt. Relative humidity averages only 37%. Vegetation is sparse in the oasis and previously only poorly investigated. Two lichen species and no bryophytes were known from the area. In November-December 2018, a survey of terrestrial flora and vegetation was made. The list of lichens was completed for the area, bryophytes were found for the first time, and some terrestrial algae were collected. In total, 23 lichen species, 1 lichenicolous fungus, 1 moss, and 18 terrestrial algae were discovered for the locality. The abundance of each species within their habitats was also evaluated. The lichen flora of the Untersee Oasis is typical for continental oases and similar to other previously investigated internal territories of Dronning Maud Land, except for the very rich lichen flora of the Schirmacher Oasis. Key words: Queen Maud Land, Schirmacher Oasis, biodiversity, vegetation, flora, taxonomy, lichen biota, mosses DOI: 10.5817/CPR2020-2-16 ——— Received July 31, 2020, accepted December 2, 2020. *Corresponding author: M. Andreev <[email protected]> Acknowledgements: Primary support for research was provided by the Tawani Foundation of Chicago, the Trottier Family Foundation, NASA’s Exobiology and Astrobiology Programs, Arctic and Antarctic Research Institute/Russian Antarctic Expedition’s Subprogram ‘‘Study and Research of the Antarctic’’ of the Federal Target Program ‘‘World Ocean.’’, partly by the Russian Foundation of Fundamental Sciences (18-04-00900, 19-54-18003), and by the research project of the Komarov Botanical Institute RAS (АААА-А18-118022090078-2). Logistics support was provided by Antarctic Logistics Centre International (ALCI), Cape Town, South Africa. Microphotographs of algae were taken using equipment of the Core Facility Center “Cell and Molecular Technologies in Plant Science” at the Komarov Botanical Institute of the Russian Academy of Sciences (St. Petersburg, Russia). In particular we thank reviewer Ole William Purvis (Natural History Museum, London) for his constructive comments and suggestions on earlier version of this manuscript. 203 M. ANDREEV et al. Introduction Wohlthat Massif is situated in the cen- (Otto-von-Gruber-Gebirge). The Untersee tral part of Dronning Maud Land (Queen Oasis (Fig. 1) with two ice covered lakes – Maud Land) between 11°E and 14°E and Untersee and Obersee, is situated in the ca. 200 km south of the barrier of Novo- alpine high mountain region of Gruber lazarevskaya Ice Shelf. It consists of the Mts. It covers an area ca 15 km lying east- Humboldt Mts., several North-South facing west and 20-25 km towards the north- ridges of the Petermann Ranges and the south (Haendel and Kaup 1986). generally East-West facing Gruber Mts. Fig. 1. Sketch map of the study area with the location of Lake Untersee, central Dronning Maud Land, East Antarctica. Altitude is given in meters above sea level (Wand et al. 1997). Lake Untersee is located at 71° 20’ S et al. 2011). The lake arose from a melt- and 13° 45’ E at an altitude of 563 m a. s. l. water pond during climatic optimum peri- and covers a surface area of 11.4 km2 ods in the Holocene. Ice cover has ranged (6.5 km long and 2.5 km wide) (Fig. 2, 3). in thickness from 2.2 to 3.8 m over time. It is one of the largest and deepest (>160 m Lake Obersee (3.43 km2), located 7 km deep) perennially ice-covered ultraoligotro- north-eastern of the lake Untersee, is com- phic freshwater lakes in continental Ant- paratively shallow with a depth less than arctica (Hermichen et al. 1985, Andersen 20 m. 204 FLORA OF LAKE UNTERSEE OASIS, ANTARCTICA Fig. 2. Wohlthat Massiv, Gruber Mountains and Lake Untersee Oasis (Dronning Maud Land, East Antarctica). ([1]-Map Wohlthatmassivet, Fimbulheimen, Sheet M5. Norsk Polarinstitutt, Oslo, 1968). Lake Untersee lies in the basin of a deep 7,000 years (Simonov et al. 1985). Since cirque-like glacial trough valley which is that time, the area has been free of ice and open to the North and surrounded on its the climate relatively stable. eastern, southern, and western sides by The mean annual temperature at Lake the high Gruber Mts. (central Wohlthat Untersee was determined to be –10.6° ± Massif). The southern main crest reaches 0.6°C. The average wind speed recorded nearly 3,000 m a. s. l. (Ritscher Peak – was 5.4 ms-1 and maximum 35.7 ms-1. 2,810 m). The mean elevation of the polar Strong winds are associated with katabatic plateau around the lake is ca. 1,000 m. flows from the south. The dominant wind Steep, partly moraine-covered mountain direction for strong winds is from the south slopes (up to 300-400 m high from the during all seasons, with a secondary source present lake’s level) surround the remain- in the summer from the East-Northeast. ing sides of the lake (Simonov et al. 1985). Relative humidity averages at 37%. Low The cirque of Lake Untersee was formed summer temperatures and high wind speeds around 58,000 yr BP, as a result of deep create conditions resulting in a local cli- ice scouring (Stackebrandt 1995). The last mate that is dominated by intense evapo- ice retreat began between 12,000 and ration and sublimation but with little melt 10,000 yr BP. The present geomorphologi- (Andersen et al. 2015). cal situation has existed for approximately 205 M. ANDREEV et al. Fig. 3. Lake Untesee and Mt. Bastei. View towards NEE into the Untesee depression. (Photo: M. Andreev). The area of the northeastern part of in the western part of Dronning Maud Land central Dronning Maud Land including the (Bowra et al. 1966, Lindsay 1971, 1972; Schirmacher Oasis, Wohlthat Massif and Lindsay and Brook 1971, Ryan et al. 1989, other inland mountain ridges, was first in- Thor 1995), and in Sør Rondane in the east- vestigated and mapped in 1939 from the ern part (Dodge 1962). Contemporary the air by pilots of the German Antarctic Ex- first botanical collections from Dronning pedition (Bormann and Fritzsche 1995). Maud Land were obtained by the Komarov In 1949-1952 the British Swedish Nor- Botanical Institute (St. Petersburg, Russia). wegian Antarctic expedition and later in N. S. Golubkova studied lichens from the 1958-1959 Norwegian Antarctic Expedi- Schirmacher Oasis, collected by I. M. Si- tion were undertaken in the western part of monov in 1962-1963 and 1965-1966 (Go- Dronning Maud Land. The main regular lubkova and Savicz 1965, 1966; Golubkova observations and the first systematic geo- and Simonov 1972). One newly described graphical and geological investigations of moss species from the Schirmacher Oa- the region, including the Wohlthat Massif, sis was reported by Savicz-Lyubitskaya were carried out by the 4th–6th Soviet Ant- and Smirnova (1964). The other authors arctic Expeditions ([2] - Atlas Antarktiki (Aleshinskaya and Bardin 1965) reported 1969, Bormann and Fritzsche 1995). varieties of algae determined in water sam- The first botanical specimens were col- ples taken from lakes of the Schirmacher lected in the 1950-60’s during expeditions Oasis. 206 FLORA OF LAKE UNTERSEE OASIS, ANTARCTICA Lake Untersee Oasis has repeatedly collections by G. T. Bowra in Heimefront- attracted scientific interest during recent fjella in 1963-1964 were redetermined by years (Kaup et al. 1988, Richter and Bor- G. Thor, who has studied the materials mann 1995), but because of its remote lo- of the Swedish expedition of 1991-1992 cation it has received much less attention as well. In total, 16 lichen and two moss than other areas in this part of the Ant- species were found (Thor 1995). Lichens arctic continent. In January/February 1969, of Sverdrup Mountains were studied by the first traverse to the Untersee Oasis area Øvstedal (1983a) on the basis of speci- was made by the 14th Soviet Antarctic mens collected by J. Angard during the Expedition team and the first geographic- Norwegian Antarctic Expedition (1970- geological and hydrological study of the 1971). Lichens collected during the British- area was made (Kosenko and Kolobov Swedish-Norwegian Antarctic Expedition 1970). The joint Soviet-German team led to the internal areas of Dronning Maud by I. M. Simonov investigated the area Land in 1949-1952 were studied by Øvste- in 1983 (Klokov et al. 1987) and carried dal (1986) and 23 species recorded. Biolog- out limnological, paleoenvironmental and ical survey of the Robertskollen nunataks geological studies of the Wohlthat Massif was undertaken by the South African Ant- (Kaup et al. 1988). During the 1970-90’s, arctic Expedition during the summer of German scientists studied the Schirmacher 1987-1988 (Ryan et al. 1989). Provisional and the Untersee Oases areas. The latter classification of plant communities in the one was just briefly investigated. They car- Gjelsvikfjella and Mühlig-Hofmannfjella ryied out floristic studies of algae, lichens Mts. was proposed by Engelskjøn (1985, and bryophytes. Since 1983, geologists of 1986). the former German Democratic Republic In the eastern part of Dronning Maud have made three expeditions to the region, Land, Dodge (1962) recorded 10 lichen the first of which was a joint Soviet- species from Sør Rondane mountains ca.
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