Survey of Algae and Other Terrestrial Biota at Edward VII Peninsula, Marie Byrd Land

Total Page:16

File Type:pdf, Size:1020Kb

Survey of Algae and Other Terrestrial Biota at Edward VII Peninsula, Marie Byrd Land Antarctic Science 1 (3):2 15-224 (1989) Survey of algae and other terrestrial biota at Edward VII Peninsula, Marie Byrd Land PAUL A. BROADY Department of Plant and Microbial Sciences, University of Canterbury, Private Bag. Christchurch I,New Zealand Abstract: The survey concentrated on algal communities but also gathered information on mosses, lichens andmicrofauna. All 23 nunataks in theRockefellerandAlex~dramountains(77000'-78030'S,152"-154OW) were visited, including ones both with and without nutrient enrichment from bird colonies. Over 30 species of algae were recorded with Cyanobactena and Chlorophyta dominant as in other regions of continental Antarctica. Diatoms were not found. The most frequent algae were Cyanothece aeruginosa, Gloeocapsa spp., Oscillatoriaceae, Nostoc sp., Pseudococcomyxa simplex, Stichococcus bacillaris, cf. Desmococcus vulgaris, Prasiola crispa and Prasiococcus caicarius. Although lichens were the most visually prominent vegetation, free-living algae occurred in the widespread 'non-aquatic' habitats as epilithic,chasmoendoli thic andedaphic communities as well as being epiphytic on the sparse moss cushions. Aquatic habitats were few and there were only three small pondson or adjacent tonunataks. On ablating ice, cryoconitepondscontained Homoeothrix cf. rivularis, recorded for the first time in Antarctica. Preliminary identifications show 23 species of lichens and six species of mosses. No mites and collembola were seen. Samples contained testate amoebae, ciliate protozoa, rotifers and tardigrades but no nematodes. Received 30 December 1988, accepted 10 March 1989 Key words: Antarctica, ecology, microfauna, nunataks, vegetation. Introduction The majority of terrestrial biological research in continental Antarctica has been performed at coastal ice-free regions with good access from research stations, for instance in the dry valleys of southern Victoria Land and on Ross Island (e.g. Friedmann 1982, Broady 1989), at the Vestfold Hills (Pickard 1986) andin thevicinity of Syowa station, Liitzow- Holm Bay (e.g. Oguni et al. 1987). However, there is increasing interest in the more remote nunataks, e.g. Mount Kobourg, northern Victoria Land (Kappen 1985) and in Dronning Maud Land (Engelskjon 1986, Pankow et al. 1987, Ryan & Watkins, in press). Wide-ranging observations and collections were made during a combined geological and biological expedition to nunataks on Edward VII Peninsula (77°00-78"30S, 152"- 154"W), Marie ByrdLand (Fig. 1) during summer 1987-88. 1 Reported here are observationson the algae, mosses, lichens Fig. 1. Location of Edward VII Peninsula and other regions and microfauna. A description of the ornithology has been mentioned in the text. 1-3 = Marie Byrd Land, 1 = Edward published elsewhere (Broady et a/. 1989). VII Peninsula, 2 = Edsel Ford Ranges, 3 = Ames and Flood Reports on the terrestrial biology of Edward VII Peninsula ranges, 4 = Horlick Mountains, 5 = Ellsworth Mountains, are few and lack detail. Early reports of mosses and lichens 6-8 = Dronning Maud Land, 6 = Robertskollen, were made by Presuud (in Amundsen 1912, p. 249), Gould 7 = Gjelsvikfjella and Miihlig-Hofmannfjella, (1931, p. 20) and Siple (1938, p. 490). The last author 8 = Unterseeoase, 9 =Liitzow-Holm Bay, 10 = Mawson Rock, 11 = Framnes Mountains, 12 = Vestfold Hills, reported mainly on more detailed studies made in Edsel Ford 13-14 = northern Victoria Land, 13 = Mount Kobourg, Ranges, 130 km further east (77"S, 145"W). Lichens were Birthday Ridge, 14 = Edmondson Point, Cape Washington, described by Dodge & Baker (1938) and mosses by Baruam Campbell Glacier, Inexpressible Island, 15 = southern (1938). Perkins(1945,p. 282) sampledplantsfrom 11 peaks Victoria Land dry valleys, 16 = McMurdo Ice Shelf, in Rockefeller Mountains. Lichens in these collections were 17 = Ross Island, 18 = Shackleton Glacier. 21 5 http://journals.cambridge.org Downloaded: 03 Mar 2015 IP address: 169.229.32.36 21 6 P.A. BROADY identified by Dodge (1973). Rudolph (1967) collected granites and metasediments. A general description of the lichens and noted an absence of microarthropods on region has been provided by Wade (1945) and a 1:250 000 Washington Ridge. Thisis theonly commenton microfauna map is available (United States Geological Survey 1972). although in eastern Marie Byrd Land, Siple (1938, p. 495) On 47 days in the field, during early to mid-summer, found protozoa, rotifers and tardigrades in pond water, and meteorological observations were taken twice a day at Strandtmann (1978,1981) described a new species of mite. approximately 1000and 2230 h solar time. The air tempera- ture ranged from -1 7" to -2°C but on 82% of occasions was between -10" to -3°C. There were 6-8 oktas of cloud on Description of the region 76% of observations. Wind was frequent but did not exceed 20 kn. Conditions were calm for 13% of observations, The seven nunataks of the Alexandra Mountains and the 16 winds were <10 kn for 68% and >10 kn for 19%. The of theRockefeller Mountains are the only ice-free land in the prevailing wind was from east to north-east. Snowfall or Edward VII Peninsula, and comprise less than 0.5% of the snowdrift occurred on 25 days. total area (Fig. 2). They are typical nunataks of the 'Conti- nental Ice Slope' region as defined by Pickard & Seppelt (1984, p. 88, fig. 10). There are no coastal outcrops. Scott Methods and materials Nunataks are closest to the coast and are 11 km inland. Mount Paterson is furthest inland, 86 km from the coast. Exposed rock was reached at all nunataks except Mount Summits range from about 419 m to 1174 m altitude and, Manger where it was inaccessible. Efforts were made to except close to the coast, the surrounding ice-surfaces have collect the full diversity of vegetation at each nunatak. an elevation of 400 m to over 1000 m. The most extensive Samples of algae and substratum were collected into sterile nunataks, Mount Paterson and Washington Ridge in polythene bags using clean instruments. In the field, speci- Rockefeller Mountains (Figs 3-5), are low ridges up to 3 km mens were kept at ambient temperatures and were buried in long. Ice-free rock in Alexandra Mountains is much less snow at campsites. Field searches were made for mites and extensive and is mostly steep slopes and cliffs of two N-NE collembola using a lox hand-lens in likely habitats but no facing escarpments. The rocks of both ranges comprise extraction procedures were used. Transport to New Zealand and subsequent storage was at -20°C. Taxonomy of cyanobacteria follows the system of Geitier (1932). Identifications of ciliate protozoa have been made ROSS by Dr W. Foissner (Universiat Salzburg). Rotifers and SEA t11.45 MtLBlRT ROCKS SlRIOtR ROCKS MT PATERSON 77'30' EOWARO VII 0 +q-& .\MA 4.5.6.19.20.37 C'L 3 i PENINSULA \ Ill SCHLOSSBhCH i 22 50 PETREL 2.39 k23,38 4 46, FOKKLR ROCKS AE[KINRIDGt PK b ROCKEFELLER Ills \ Wr FRANKLIN' q5' km 906. WASHINGTON RIDGE Fig. 2. Geographical features of Edward VII Peninsula, Mane Byrd Land. Inset shows the location of Edward VII Peninsula 48,L9,4 in the south-east comer of Ross Sea. Nunataks of the MELT /d*30 Alexandra and Rockefeller mountains are shown as follows: N FLOW I 0 km 2 h SN = Scott Nunataks, SW = Mount Swadener, BO = Bowman L__ Peak, MA = Mount Manger, JO = Mount Josephine, CL = LAKE Clarke Peak, LG = La Gorce Peak, DR = Drummond Peak, FR = Mount Frazier, JA = Mount Jackling, FZ = Mount Fig. 3. Nunataks in the central Rockefeller Mountains, Mount Fitzsimmons, SH = Mount Shideler, PA = Mount Paterson Paterson and Washington Ridge are shown in Figs 4 and 5 (see Fig. 4), GO = Gould Peak, BU = Mount Butler, TE = respectively. Proglacial lakes and position of the Antarctic Tennant Peak. Nunataks to the east of Mount Paterson are petrel colony are indicated. Inset gives location (also see Fig. shown in more detail in Fig. 3. 2). Numbers refer to samples (see Tables i1-IV). http://journals.cambridge.org Downloaded: 03 Mar 2015 IP address: 169.229.32.36 MARIE BYRD LAND ALGAE AND OTHER TERRESTRIAL BIOTA 21 7 Table I. Algae obselved in microscopic examination of 53 samples and subjective estimates of their abundance. 9% of occurrence and Algae abundance in all samples rare occ. freq. abund. TG - Cyanobacteria Aphanocapsa eiachista West & West 1 2 Chroococcus minor (Kuetz.) Naeg. 1 2 Chroococcus turgidus (Kuetz.) Naeg. 1 2 Cyanothece aeruginosa (Naeg.) Komarek 3 1 4 2 19 Gloeocapsa aipina Naeg. 2 1 18 Gioeocapsa kuetzingiana Naeg. 2 3 1 11 Gioeocapsa cf. punctata Naeg. 1 1 28 Gloeocapsa ralfsiana Kuetz. 2 1 2 1 11 Fig. 4. An aerial view of Mount Paterson taken from the north- cf. Chroococcidiopsis sp. 1 14 west at an altitude of about 1000 m. The nunatak is about Crinalium cf. magnum Fritsch & John 1 2 2.8 km lone. Oscillatoriaceae, trichomes 1-2 pm wide 2 16 Phormidium autumnale (Ag.) Gom. 2 2 1 9 Phormldium cf.fragiie (Menegh.) Gom. 1 2 Phormidium cf. laminosum Gom. 1 4 3 15 Schizothrir cf. antarctica Fritsch 12 Calothrir cf. parietina (Naeg.) Thuret 1 3 8 Homoeothrix cf. rivularis (Hansg.) Komarek & Kann 36 Nostoc sp. 1 1 3 5 19 Toiypothrix cf. bouteiilei (Breb. & Desm.) Forti 1 1 4 Stigonema minutum (Ag.) Hassall 1 26 Chlorophyta cf. Chioreiia SQ. 2 4 cf. Chlorococcum sp. 1 2 cf. Coenocystis sp. 1 2 1 3 13 cf. Dicfyochloropsis sp. 1 26 Pseudococcomyxa simplex (Mainx) Fott 4 5 17 view looking north along Washington Ridge from the Fig. 5. A Unidentified unicells 2 3 3 1 17 southernmost rock exposure. A frozen pond, which is Lichen gonidia with unicells 1 5 4 19 approximately 10 m long, can be seen in a windscoop in the Stichococcus baciilaris Naeg. 5 3 11 3 42 middle distance. cf. Desmococcus vulgaris Brand 2 3 5 14 45 Prasioia caiophyila (Carmich.) Menegh.
Recommended publications
  • Antarctic Bryophyte Research—Current State and Future Directions
    Bry. Div. Evo. 043 (1): 221–233 ISSN 2381-9677 (print edition) DIVERSITY & https://www.mapress.com/j/bde BRYOPHYTEEVOLUTION Copyright © 2021 Magnolia Press Article ISSN 2381-9685 (online edition) https://doi.org/10.11646/bde.43.1.16 Antarctic bryophyte research—current state and future directions PAULO E.A.S. CÂMARA1, MicHELine CARVALHO-SILVA1 & MicHAEL STecH2,3 1Departamento de Botânica, Universidade de Brasília, Brazil UnB; �[email protected]; http://orcid.org/0000-0002-3944-996X �[email protected]; https://orcid.org/0000-0002-2389-3804 2Naturalis Biodiversity Center, P.O. Box 9517, 2300 RA Leiden, Netherlands; 3Leiden University, Leiden, Netherlands �[email protected]; https://orcid.org/0000-0001-9804-0120 Abstract Botany is one of the oldest sciences done south of parallel 60 °S, although few professional botanists have dedicated themselves to investigating the Antarctic bryoflora. After the publications of liverwort and moss floras in 2000 and 2008, respectively, new species were described. Currently, the Antarctic bryoflora comprises 28 liverwort and 116 moss species. Furthermore, Antarctic bryology has entered a new phase characterized by the use of molecular tools, in particular DNA sequencing. Although the molecular studies of Antarctic bryophytes have focused exclusively on mosses, molecular data (fingerprinting data and/or DNA sequences) have already been published for 36 % of the Antarctic moss species. In this paper we review the current state of Antarctic bryological research, focusing on molecular studies and conservation, and discuss future questions of Antarctic bryology in the light of global challenges. Keywords: Antarctic flora, conservation, future challenges, molecular phylogenetics, phylogeography Introduction The Antarctic is the most pristine, but also most extreme region on Earth in terms of environmental conditions.
    [Show full text]
  • Number 90 RECORDS of ,THE UNITED STATES ANTARCTIC
    ~ I Number 90 RECORDS OF ,THE UNITED STATES ANTARCTIC SERVICE Compiled by Charles E. Dewing and Laura E. Kelsay j ' ·r-_·_. J·.. ; 'i The National Archives Nat i on a 1 A r c hive s and R e c o rd s S e r vi c e General Services~Administration Washington: 1955 ---'---- ------------------------ ------~--- ,\ PRELIMINARY INVENTORY OF THE RECORDS OF THE UNITED STATES ANTARCTIC SERVICE {Record Group 1 Z6) Compiled by Charles E. Dewing and Laura E. Kelsay The National Archives National Archives and Records Service General Services Administration Washington: 1955 National Archives Publication No. 56-8 i\ FORENORD To analyze and describe the permanently valuable records of the Fed­ eral Government preserved in the National Archives Building is one of the main tasks of the National Archives. Various kinds of finding aids are needed to facilitate the use of these records, and the first step in the records-description program is the compilation of preliminary inventories of the material in the 270-odd record groups to which the holdings of the National Archives are allocated. These inventories are called "preliminary" because they are provisional in character. They are prepared.as soon as possible after the records are received without waiting to screen out all disposable material or to per­ fect the arrangement of the records. They are compiled primarily for in­ ternal use: both as finding aids to help the staff render efficient refer­ ence service and as a means of establishing administrative control over the records. Each preliminary inventory contains an introduction that briefly states the history and fUnctions of the agency that accumulated the records.
    [Show full text]
  • Ice Caves of Terra Nova Bay (Victoria Land, Antarctica)
    SPECIALE GLACIER CAVES NIMBUS 23-24 Ice Caves of Terra Nova Bay (Victoria Land, Antarctica) Mirco Meneghel - Dipartimento di Geografia, University of Padova, Italy Giovanni Badino - Dipartimento di Fisica Generale, University of Torino, Italy Associazione La Venta Abstract Baia Terra Nova, sulla costa occi- wider Terra Nova Bay, on the we- In the 2000/2001 expedition of dentale del Mare di Ross. Sono stern coast of the Ross Sea, at 74° the Italian Programme of Resear- state esplorate tre grotte nella 41' 42" S lat. and 164° 07' 23" E ch in Antarctica (PNRA) an inve- fronte dei ghiacciai al contatto col long. The Transantarctic Mts, stigation on the presence of ca- mare e un'altra sulla sommità del whose relief is often higher than ves in ice has been carried out monte Melbourne, un cono vulca- 3000 m, fringe the coast. South near the Italian Station of Terra nico di 2700 metri di altezza. Le of the Base the mountain chaine Nova Bay, on the western coast of grotte sulla costa sono crepacci is crossed by outlet glaciers that the Ross Sea (Northern Victoria ampliati dalla sublimazione del drain the ice of the inlandsis. On Land). Three caves have been ex- ghiaccio a causa della differenza the north huge valley glaciers plored at the snout of glaciers di temperatura fra il ghiaccio e flow from the mountains to the reaching the sea and an other l'acqua marina. La grotta subgla- sea. The Italian Base is placed one on the summit of Mt Mel- ciale sul monte Melbourne è ge- between the region of the Dry bourne, a volcanic cone 2700 m nerata dal calore delle rocce vul- Valleys to the south, where broad 1 - Below - high.
    [Show full text]
  • Management Plan for Antarctic Specially Protected Area No. 116 NEW COLLEGE VALLEY, CAUGHLEY BEACH, CAPE BIRD, ROSS ISLAND
    Management Plan For Antarctic Specially Protected Area No. 116 NEW COLLEGE VALLEY, CAUGHLEY BEACH, CAPE BIRD, ROSS ISLAND 1. Description of values to be protected In 1985, two areas at Cape Bird, Ross Island were designated as SSSI No. 10, Caughley Beach (Recommendation XIII-8 (1985)) and SPA No. 20, New College Valley (Recommendation XIII-12 (1985)), following proposals by New Zealand that these areas should be protected because they contained some of the richest stands of moss and associated microflora and fauna in the Ross Sea region of Antarctica. This is the only area on Ross Island where protection is specifically given to plant assemblages and associated ecosystems. At that time, SPA No. 20 was enclosed within SSSI No. 10, in order to provide more stringent access conditions to that part of the Area. In 2000, SSSI No. 10 was incorporated with SPA No. 20 by Measure 1 (2000), with the former area covered by SPA No. 20 becoming a Restricted Zone within the revised SPA No. 20. The boundaries of the Area were revised from the boundaries in the original recommendations, in view of improved mapping and to follow more closely the ridges enclosing the catchment of New College Valley. Caughley Beach itself was adjacent to, but never a part of, the original Area, and for this reason the entire Area was renamed as New College Valley, which was within both of the original sites. The Area was redesignated by Decision 1 (2002) as Antarctic Specially Protected Area (ASPA) No. 116 and a revised Management Plan was adopted through Measure 1 (2006).
    [Show full text]
  • JOURNAL Number Six
    THE JAMES CAIRD SOCIETY JOURNAL Number Six Antarctic Exploration Sir Ernest Shackleton MARCH 2012 1 Shackleton and a friend (Oliver Locker Lampson) in Cromer, c.1910. Image courtesy of Cromer Museum. 2 The James Caird Society Journal – Number Six March 2012 The Centennial season has arrived. Having celebrated Shackleton’s British Antarctic (Nimrod) Expedition, courtesy of the ‘Matrix Shackleton Centenary Expedition’, in 2008/9, we now turn our attention to the events of 1910/12. This was a period when 3 very extraordinary and ambitious men (Amundsen, Scott and Mawson) headed south, to a mixture of acclaim and tragedy. A little later (in 2014) we will be celebrating Sir Ernest’s ‘crowning glory’ –the Centenary of the Imperial Trans-Antarctic (Endurance) Expedition 1914/17. Shackleton failed in his main objective (to be the first to cross from one side of Antarctica to the other). He even failed to commence his land journey from the Weddell Sea coast to Ross Island. However, the rescue of his entire team from the ice and extreme cold (made possible by the remarkable voyage of the James Caird and the first crossing of South Georgia’s interior) was a remarkable feat and is the reason why most of us revere our polar hero and choose to be members of this Society. For all the alleged shenanigans between Scott and Shackleton, it would be a travesty if ‘Number Six’ failed to honour Captain Scott’s remarkable achievements - in particular, the important geographical and scientific work carried out on the Discovery and Terra Nova expeditions (1901-3 and 1910-12 respectively).
    [Show full text]
  • Federal Register/Vol. 84, No. 78/Tuesday, April 23, 2019/Rules
    Federal Register / Vol. 84, No. 78 / Tuesday, April 23, 2019 / Rules and Regulations 16791 U.S.C. 3501 et seq., nor does it require Agricultural commodities, Pesticides SUPPLEMENTARY INFORMATION: The any special considerations under and pests, Reporting and recordkeeping Antarctic Conservation Act of 1978, as Executive Order 12898, entitled requirements. amended (‘‘ACA’’) (16 U.S.C. 2401, et ‘‘Federal Actions to Address Dated: April 12, 2019. seq.) implements the Protocol on Environmental Justice in Minority Environmental Protection to the Richard P. Keigwin, Jr., Populations and Low-Income Antarctic Treaty (‘‘the Protocol’’). Populations’’ (59 FR 7629, February 16, Director, Office of Pesticide Programs. Annex V contains provisions for the 1994). Therefore, 40 CFR chapter I is protection of specially designated areas Since tolerances and exemptions that amended as follows: specially managed areas and historic are established on the basis of a petition sites and monuments. Section 2405 of under FFDCA section 408(d), such as PART 180—[AMENDED] title 16 of the ACA directs the Director the tolerance exemption in this action, of the National Science Foundation to ■ do not require the issuance of a 1. The authority citation for part 180 issue such regulations as are necessary proposed rule, the requirements of the continues to read as follows: and appropriate to implement Annex V Regulatory Flexibility Act (5 U.S.C. 601 Authority: 21 U.S.C. 321(q), 346a and 371. to the Protocol. et seq.) do not apply. ■ 2. Add § 180.1365 to subpart D to read The Antarctic Treaty Parties, which This action directly regulates growers, as follows: includes the United States, periodically food processors, food handlers, and food adopt measures to establish, consolidate retailers, not States or tribes.
    [Show full text]
  • Bibliography of Publications 1974 – 2019
    W. SZAFER INSTITUTE OF BOTANY POLISH ACADEMY OF SCIENCES Ryszard Ochyra BIBLIOGRAPHY OF PUBLICATIONS 1974 – 2019 KRAKÓW 2019 Ochyraea tatrensis Váňa Part I. Monographs, Books and Scientific Papers Part I. Monographs, Books and Scientific Papers 5 1974 001. Ochyra, R. (1974): Notatki florystyczne z południowo‑wschodniej części Kotliny Sandomierskiej [Floristic notes from southeastern part of Kotlina Sandomierska]. Zeszyty Naukowe Uniwersytetu Jagiellońskiego 360 Prace Botaniczne 2: 161–173 [in Polish with English summary]. 002. Karczmarz, K., J. Mickiewicz & R. Ochyra (1974): Musci Europaei Orientalis Exsiccati. Fasciculus III, Nr 101–150. 12 pp. Privately published, Lublini. 1975 003. Karczmarz, K., J. Mickiewicz & R. Ochyra (1975): Musci Europaei Orientalis Exsiccati. Fasciculus IV, Nr 151–200. 13 pp. Privately published, Lublini. 004. Karczmarz, K., K. Jędrzejko & R. Ochyra (1975): Musci Europaei Orientalis Exs‑ iccati. Fasciculus V, Nr 201–250. 13 pp. Privately published, Lublini. 005. Karczmarz, K., H. Mamczarz & R. Ochyra (1975): Hepaticae Europae Orientalis Exsiccatae. Fasciculus III, Nr 61–90. 8 pp. Privately published, Lublini. 1976 006. Ochyra, R. (1976): Materiały do brioflory południowej Polski [Materials to the bry‑ oflora of southern Poland]. Zeszyty Naukowe Uniwersytetu Jagiellońskiego 432 Prace Botaniczne 4: 107–125 [in Polish with English summary]. 007. Ochyra, R. (1976): Taxonomic position and geographical distribution of Isoptery‑ giopsis muelleriana (Schimp.) Iwats. Fragmenta Floristica et Geobotanica 22: 129–135 + 1 map as insertion [with Polish summary]. 008. Karczmarz, K., A. Łuczycka & R. Ochyra (1976): Materiały do flory ramienic środkowej i południowej Polski. 2 [A contribution to the flora of Charophyta of central and southern Poland. 2]. Acta Hydrobiologica 18: 193–200 [in Polish with English summary].
    [Show full text]
  • Fault Kinematic Studies in the Transantarctic Mountains, Southern Victoria Land TERRY J
    studies. Together these data will be used to develop a model to plate tectonic modeling. In R.A. Hodgson, S.P. Gay, Jr., and J.Y. of the structural architecture and motion history associated Benjamins (Eds.), Proceedings of the First International Conference with the Transantarctic Mountains in southern Victoria Land. on the New Basement Tectonics (Publication number 5). Utah Geo- logical Association. We thank Jane Ferrigno for cooperation and advice on Lucchita, B.K., J. Bowell, K.L. Edwards, E.M. Eliason, and H.M. Fergu- image selection; John Snowden, David Cunningham, and son. 1987. Multispectral Landsat images of Antarctica (U.S. Geo- Tracy Douglass at the Ohio State University Center for Map- logical Survey bulletin 1696). Washington, D.C.: U.S. Government ping for help with computer processing; and Carolyn Merry, Printing Office. Gary Murdock, and Ralph von Frese for helpful discussions Wilson, T.J. 1992. Mesozoic and Cenozoic kinematic evolution of the Transantarctic Mountains. In Y. Yoshida, K. Kaminuma, and K. concerning image analysis. This research was supported by Shiraishi (Eds.), Recent progress in antarctic earth science. Tokyo: National Science Foundation grant OPP 90-18055 and by the Terra Scientific. Byrd Polar Research Center of Ohio State University. Wilson, T.J. 1993. Jurassic faulting and magmatism in the Transantarctic Mountains: Implication for Gondwana breakup. In R.H. Findlay, M.R. Banks, R. Unrug, and J. Veevers (Eds.), Gond- References wana 8—Assembly, evolution, and dispersal. Rotterdam: A.A. Balkema. Wilson, T.J., P. Braddock, R.J. Janosy, and R.J. Elliot. 1993. Fault kine- Isachsen, Y.W. 1974.
    [Show full text]
  • Terra Nova Bay, Ross Sea
    MEASURE 14 - ANNEX Management Plan for Antarctic Specially Protected Area No 161 TERRA NOVA BAY, ROSS SEA 1. Description values to be protected A coastal marine area encompassing 29.4km2 between Adélie Cove and Tethys Bay, Terra Nova Bay, is proposed as an Antarctic Specially Protected Area (ASPA) by Italy on the grounds that it is an important littoral area for well-established and long-term scientific investigations. The Area is confined to a narrow strip of waters extending approximately 9.4km in length immediately to the south of the Mario Zucchelli Station (MZS) and up to a maximum of 7km from the shore. No marine resource harvesting has been, is currently, or is planned to be, conducted within the Area, nor in the immediate surrounding vicinity. The site typically remains ice-free in summer, which is rare for coastal areas in the Ross Sea region, making it an ideal and accessible site for research into the near-shore benthic communities of the region. Extensive marine ecological research has been carried out at Terra Nova Bay since 1986/87, contributing substantially to our understanding of these communities which had not previously been well-described. High diversity at both species and community levels make this Area of high ecological and scientific value. Studies have revealed a complex array of species assemblages, often co-existing in mosaics (Cattaneo-Vietti, 1991; Sarà et al., 1992; Cattaneo-Vietti et al., 1997; 2000b; 2000c; Gambi et al., 1997; Cantone et al., 2000). There exist assemblages with high species richness and complex functioning, such as the sponge and anthozoan communities, alongside loosely structured, low diversity assemblages.
    [Show full text]
  • Downloaded 10/01/21 04:29 PM UTC 224 MONTHLY WEATHER REVIEW
    APRIL, 1914. MONTHLY WEATHER REWW. 223 of no direct consequence to lants, its importance being ordinary weather stations. Therefore it would be of urely meteorological, the reP ative huniiclit affects them great advantage to students of plant life if such deter- Zirectly, since it so largely determines t i! e amount of minations could be made at agricultural and forest exper- transpiration. The monthly , mean relative humidity iment stations.' and its minimum, and particularly the average relative Sunshine. humidity with its minimum during periods of different wind direction, are things important to know. In local- Light is another important factor in t-he development ities with a humid climate and wit,hout n, distinct hot of plants. The amount avdable for plants in a given eriod, where fogs are frequent, observations upon the 1oc.alit-y depends upon cloudiness and geographic lati- fatter should, of course, Gve all the information as to tude. For this reason, the avera. e monthly cloudi- humidit of the air necessary for the purposes of botanical ness, tjhe average cloudiness for win as of different direc- geograpE y.a tions, and the number of clear, semicloudy, and cloudy Precipitation. days should be computed. Some simple sunshine record, especially for winds of different directions, is The important part which precipitation, especially also necessary. The occurrence of days with sunshine total precipitation, plays in plant life, needs no discussion. should be given in per cent of the total number of obser- The maximum precipitation for any day during the month va tions. and the number of da s of precipitation are also inipor- Bammetric pressure.
    [Show full text]
  • Phylogeny of Three East Antarctic Mosses
    University of Wollongong Research Online University of Wollongong Thesis Collection 1954-2016 University of Wollongong Thesis Collections 2013 Phylogeny of Three East Antarctic Mosses Rhys A. Wyber University of Wollongong Follow this and additional works at: https://ro.uow.edu.au/theses University of Wollongong Copyright Warning You may print or download ONE copy of this document for the purpose of your own research or study. The University does not authorise you to copy, communicate or otherwise make available electronically to any other person any copyright material contained on this site. You are reminded of the following: This work is copyright. Apart from any use permitted under the Copyright Act 1968, no part of this work may be reproduced by any process, nor may any other exclusive right be exercised, without the permission of the author. Copyright owners are entitled to take legal action against persons who infringe their copyright. A reproduction of material that is protected by copyright may be a copyright infringement. A court may impose penalties and award damages in relation to offences and infringements relating to copyright material. Higher penalties may apply, and higher damages may be awarded, for offences and infringements involving the conversion of material into digital or electronic form. Unless otherwise indicated, the views expressed in this thesis are those of the author and do not necessarily represent the views of the University of Wollongong. Recommended Citation Wyber, Rhys A., Phylogeny of Three East Antarctic Mosses, Bachelor of Medical Biotechnology Advanced - Honours thesis, , University of Wollongong, 2013. https://ro.uow.edu.au/theses/4646 Research Online is the open access institutional repository for the University of Wollongong.
    [Show full text]
  • A Synthesis of the Antarctic Springtail Phylogeographic Record
    Insects 2011, 2, 62-82; doi:10.3390/insects2020062 OPEN ACCESS insects ISSN 2075-4450 www.mdpi.com/journal/insects/ Review Extreme Glacial Legacies: A Synthesis of the Antarctic Springtail Phylogeographic Record Angela McGaughran 1, Mark I. Stevens 2,*, Ian D. Hogg 3 and Antonio Carapelli 4 1 Max Planck Institute for Developmental Biology, Department for Evolutionary Biology, Spemannstr. 37-39/IV, Tübingen, D-72076, Germany; E-Mail: [email protected] 2 South Australian Museum, and School of Earth and Environmental Sciences, University of Adelaide, SA 5000, Adelaide, Australia 3 Centre for Biodiversity and Ecology Research, University of Waikato, Hamilton, New Zealand; E-Mail: [email protected] 4 Department of Evolutionary Biology, University of Siena, via A. Moro 2, 53100, Siena, Italy; E-Mail: [email protected] * Author to whom correspondence should be addressed; E-Mail: [email protected]; Tel.: +61-8-8207-7685; Fax: +61-8-8207-7222. Received: 23 December 2010; in revised form: 15 February 2011 / Accepted: 2 April 2011 / Published: 6 April 2011 Abstract: We review current phylogeographic knowledge from across the Antarctic terrestrial landscape with a focus on springtail taxa. We describe consistent patterns of high genetic diversity and structure among populations which have persisted in glacial refugia across Antarctica over both short (<2 Mya) and long (>10 Mya) timescales. Despite a general concordance of results among species, we explain why location is important in determining population genetic patterns within bioregions. We complete our review by drawing attention to the main limitations in the field of Antarctic phylogeography, namely that the scope of geographic focus is often lacking within studies, and that large gaps remain in our phylogeographic knowledge for most terrestrial groups.
    [Show full text]