Data

Biological evolution of Antarctic lakes

Australian Antarctic Data Centre
LAYBOURN-PARRY, JOHANNA
Viewed: [[ro.stat.viewed]] Cited: [[ro.stat.cited]] Accessed: [[ro.stat.accessed]]
ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=info:doi10.4225/15/54D0238FAF0A1&rft.title=Biological evolution of Antarctic lakes&rft.identifier=10.4225/15/54D0238FAF0A1&rft.publisher=Australian Antarctic Data Centre&rft.description=Beaver Lake, a large epishelf lake in Eastern Antarctica was sampled on two occasions during the austral summer of 2000. Two sites, one 1km offshore and another 6km offshore were sampled at intervals to depths of 40m and 110m respectively. The lake is an end member of ultra-oligotrophic lake systems with a very low carbon pool. Dissolved organic carbon concentrations ranged between 95-652 micro grams per litre. Nutrient levels were generally low with soluble reactive phosphorus ranging from undetectable to 8.4 micro grams per litre, ammonium ranged between 1.8-5.0 micro grams per litre, nitrate from undetectable to 161 micro grams per litre and nitrite 1.1-5.3 micro grams per litre. Chlorophyll a concentrations ( 0.39 - 4.38 micro grams per litre) showed an unusual distribution with the highest levels close to the lake bottom at the offshore site (110m) where the phototrophic nanoflagellates displayed strong autofluorescence. Bacterial concentrations were low, with a maximum of 7.60 x 107 per litre, as were the concentrations of heterotrophic nanoflagellates that exploit them. Primary production ranged between 19.7 - 25.49 micro grams C per litre day-1 and bacterial production from 0.32 - 1.15 micro grams C per litre day-1. In common with other continental Antarctic lakes, the system was dominated by a microbial plankton. However, a dwarf variety of the calanoid copepod, Boeckella poppei, occurred below 25m at concentrations of 3-5 per litre. The data suggest that primary production and bacterial production were not limited by nutrient availability, but by other factors e.g. in the case of bacterial production by organic carbon concentrations and primary production by low temperatures. The fields in this dataset are: Evolution Biological lake salinity depth m ciliates per litre cysts boeckella bacteria glucose glycine particulate organic carbon (POC) total organic carbon (TOC) DiAskenasia 15/2/00 sloved organic carbon (DOC) Monodinium Askenasia Strombidium Heliozoa scuticociliates Holophyra PNAN = Phototrophic nanoflagellates HNAN= heterotrophic nanoflagellates&rft.creator=LAYBOURN-PARRY, JOHANNA &rft.date=2000&rft.coverage=northlimit=-70.79; southlimit=-70.79; westlimit=68.3; eastLimit=68.3; projection=WGS84&rft.coverage=northlimit=-70.79; southlimit=-70.79; westlimit=68.3; eastLimit=68.3; projection=WGS84&rft_rights=This data set conforms to the CCBY Attribution License (http://creativecommons.org/licenses/by/4.0/). Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=ASAC_1131 when using these data.&rft_subject=biota&rft_subject=geoscientificInformation&rft_subject=inlandWaters&rft_subject=EARTH SCIENCE > TERRESTRIAL HYDROSPHERE > SURFACE WATER > SURFACE WATER FEATURES > LAKES/RESERVOIRS&rft_subject=BACTERIA/ARCHAEA&rft_subject=EARTH SCIENCE&rft_subject=BIOLOGICAL CLASSIFICATION&rft_subject=PLANKTON&rft_subject=BIOSPHERE&rft_subject=AQUATIC ECOSYSTEMS&rft_subject=ASKENASIA&rft_subject=BACTERIA&rft_subject=BIOLOGICAL&rft_subject=BOECKELLA&rft_subject=CILIATES PER LITRE&rft_subject=CYSTS&rft_subject=DEPTH M&rft_subject=DIASKENASIA 15/2/00&rft_subject=EVOLUTION&rft_subject=GLUCOSE&rft_subject=GLYCINE&rft_subject=HELIOZOA&rft_subject=HOLOPHYRA&rft_subject=LAKE&rft_subject=MONODINIUM&rft_subject=PARTICULATE ORGANIC CARBON (POC)&rft_subject=PNAN&rft_subject=PHOTOTROPHIC NANOFLAGELLATES&rft_subject=HNAN&rft_subject=HETEROTROPHIC NANOFLAGELLATES&rft_subject=SALINITY&rft_subject=SCUTICOCILIATES&rft_subject=SLOVED ORGANIC CARBON (DOC)&rft_subject=STROMBIDIUM&rft_subject=TOTAL ORGANIC CARBON (TOC)&rft_subject=TOC > Total Organic Carbon Analyzer&rft_subject=GROUND-BASED OBSERVATIONS&rft_subject=CONTINENT > ANTARCTICA > Beaver Lake&rft_subject=GEOGRAPHIC REGION > POLAR&rft_place=Hobart&rft.type=dataset&rft.language=English Access the data

Licence & Rights:

view details

This data set conforms to the CCBY Attribution License (http://creativecommons.org/licenses/by/4.0/). Please follow instructions listed in the citation reference provided at http://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=ASAC_1131 when using these data.

Access:

Open view details

These data are publicly available for download from the provided URL.

Brief description

Beaver Lake, a large epishelf lake in Eastern Antarctica was sampled on two occasions during the austral summer of 2000. Two sites, one 1km offshore and another 6km offshore were sampled at intervals to depths of 40m and 110m respectively. The lake is an end member of ultra-oligotrophic lake systems with a very low carbon pool. Dissolved organic carbon concentrations ranged between 95-652 micro grams per litre. Nutrient levels were generally low with soluble reactive phosphorus ranging from undetectable to 8.4 micro grams per litre, ammonium ranged between 1.8-5.0 micro grams per litre, nitrate from undetectable to 161 micro grams per litre and nitrite 1.1-5.3 micro grams per litre. Chlorophyll a concentrations ( 0.39 - 4.38 micro grams per litre) showed an unusual distribution with the highest levels close to the lake bottom at the offshore site (110m) where the phototrophic nanoflagellates displayed strong autofluorescence. Bacterial concentrations were low, with a maximum of 7.60 x 107 per litre, as were the concentrations of heterotrophic nanoflagellates that exploit them. Primary production ranged between 19.7 - 25.49 micro grams C per litre day-1 and bacterial production from 0.32 - 1.15 micro grams C per litre day-1. In common with other continental Antarctic lakes, the system was dominated by a microbial plankton. However, a dwarf variety of the calanoid copepod, Boeckella poppei, occurred below 25m at concentrations of 3-5 per litre. The data suggest that primary production and bacterial production were not limited by nutrient availability, but by other factors e.g. in the case of bacterial production by organic carbon concentrations and primary production by low temperatures. The fields in this dataset are: Evolution Biological lake salinity depth m ciliates per litre cysts boeckella bacteria glucose glycine particulate organic carbon (POC) total organic carbon (TOC) DiAskenasia 15/2/00 sloved organic carbon (DOC) Monodinium Askenasia Strombidium Heliozoa scuticociliates Holophyra PNAN = Phototrophic nanoflagellates HNAN= heterotrophic nanoflagellates

Issued: 2000-08-09

Data time period: 2000-02-05 to 2000-02-05

Data time period: 2000-02-15 to 2000-02-15

This dataset is part of a larger collection

Click to explore relationships graph

68.3,-70.79

68.3,-70.79

text: northlimit=-70.79; southlimit=-70.79; westlimit=68.3; eastLimit=68.3; projection=WGS84

Identifiers