Data

Ecological Relationships of Antarctic Tardigrades

Name: Ecological Relationships of Antarctic Tardigrades
Published: 2000-07-27

Australian Antarctic Data Centre

HEATWOLE, HAROLD

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ctx_ver=Z39.88-2004&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Adc&rfr_id=info%3Asid%2FANDS&rft_id=info:doi10.4225/15/57E4AB7A4F788&rft.title=Ecological Relationships of Antarctic Tardigrades&rft.identifier=10.4225/15/57E4AB7A4F788&rft.publisher=Australian Antarctic Data Centre&rft.description=An analysis of bedrock and associated soils was conducted at a series of coastal localities in East Antarctica as well as further inland in the Prince Charles Mountains. Protozoans and micrometazoans were extracted from soil samples and an assessment made of their ecological relations with each other and with soil characteristics. Mineral soils, regardless of topographic elevation and proximity to the coast, were characterised by large gravel fractions (fragments of underlying bedrock) and minimal clay fractions, implying that these soils were predominantly the products of physical weathering, with little chemical alteration. Only where humans, dogs or birds contributed organic matter were there elevated concentrations of nitrogen, phosphorus or organic matter. Generally, mineral nitrogen did not seem to have resulted from microbial mineralisation, but at some sites there was evidence that atmospheric nitrate had been concentrated by sublimination of snow. Water-soluble and dilute acid-soluble phosphorous concentrations were surprisingly high for such organically poor soils. There was a sufficiently large labile pool of common macronutrients to sustain the autotrophic activity likely to occur within the bounds of prevailing temperatures and moisture; thus nutrients are not likely to be limiting for these soil communities. There was a limited fauna. Flagellates were rare and ciliates occurred only in the coastal areas sampled, whereas amoebae were found over a greater geographic and elevational span. Micrometazoans such as rotifers, tardigrades and nematodes were more common in coastal soils than in those further inland, but occurred in soils over most of the naturally occurring range of soil moistures, acidities, nutrient levels, electrolyte levels and organic contents. Exceptions were the exclusion of rotifers from alkaline soils with high nutrient levels, and the tendency of nematodes to be absent from soils with low pH. Tardigrades were found at almost all levels of soil characterisitcs. The occurrence of these metazoan phyla under such a range of environments probably resulted from their known capacity to alternate between endurance of inclement conditions in a state of deep dormancy (anhydrobiosis), and taking advantage of ephemeral favourable conditions by temporarily resuming metabolic activity. The conditions measured in soils containing micrometazoans may merely indicate thise conditions these animals can survive while dormant, not those under which active animals can carry out vital processes. In some localities there were positive associations between various taxon-pairs of metazoans and protozoans, whereas at others their occurrences seemed to be random with respect to each other. The fields for this dataset are: TARDIGRADES site AMOEBAE bedrock type quartz garnet pyroxene homblende biotite K-feldspar plagioclase Others rock type field sample number catalogue Number material USDA texture class clay mineralology water content pH KCl pH H2O micro siemens per centimetre water solution P water solution K colour (Munsell) Total N Minimum N (KCl) NH3-N Dilute acid solution P loss on ignition (%) Ciliates nematodes associations&rft.creator=HEATWOLE, HAROLD &rft.date=2000&rft.coverage=northlimit=-67.5833; southlimit=-71.4166; westlimit=62.8166; eastLimit=78.0; projection=WGS84&rft.coverage=northlimit=-67.5833; southlimit=-71.4166; westlimit=62.8166; eastLimit=78.0; 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_354 when using these data.&rft_subject=biota&rft_subject=ANIMALS/INVERTEBRATES&rft_subject=EARTH SCIENCE&rft_subject=BIOLOGICAL CLASSIFICATION&rft_subject=POPULATION DYNAMICS&rft_subject=BIOSPHERE&rft_subject=ECOLOGICAL DYNAMICS&rft_subject=SPECIES/POPULATION INTERACTIONS&rft_subject=AMOEBAE&rft_subject=ANHYDROBIOSIS&rft_subject=ASSOCIATIONS&rft_subject=BEDROCK TYPE&rft_subject=BIOTITE&rft_subject=CATALOGUE NUMBER&rft_subject=CILIATES&rft_subject=CLAY MINERALOLOGY&rft_subject=COLOUR (MUNSELL)&rft_subject=DILUTE ACID SOLUTION P&rft_subject=FIELD SAMPLE NUMBER&rft_subject=GARNET&rft_subject=HOMBLENDE&rft_subject=K-FELDSPAR&rft_subject=LOSS ON IGNITION (%)&rft_subject=MATERIAL&rft_subject=MICROMETAZOAN&rft_subject=MINIMUM N (KCL)&rft_subject=NEMATODES&rft_subject=NH3-N&rft_subject=OTHERS&rft_subject=PH H2O&rft_subject=PH KCL&rft_subject=PLAGIOCLASE&rft_subject=PYROXENE&rft_subject=QUARTZ&rft_subject=ROCK TYPE&rft_subject=SITE&rft_subject=SOIL&rft_subject=TARDIGRADES&rft_subject=TOTAL N&rft_subject=USDA TEXTURE CLASS&rft_subject=WATER CONTENT&rft_subject=WATER SOLUTION K&rft_subject=WATER SOLUTION P&rft_subject=Radiometers&rft_subject=XRD > X-ray Diffractometer&rft_subject=FIELD SURVEYS&rft_subject=FIELD INVESTIGATION&rft_subject=CONTINENT > ANTARCTICA > Prince Charles Mountains&rft_subject=CONTINENT > ANTARCTICA > Else Platform&rft_subject=CONTINENT > ANTARCTICA > Jetty Peninsula&rft_subject=CONTINENT > ANTARCTICA > Pagodroma Gorge&rft_subject=CONTINENT > ANTARCTICA > Blustery Cliffs&rft_subject=CONTINENT > ANTARCTICA > Mt Woinarski&rft_subject=CONTINENT > ANTARCTICA > Mt Jacklyn&rft_subject=CONTINENT > ANTARCTICA > Moore Pyramid&rft_subject=CONTINENT > ANTARCTICA > Farley Massif&rft_subject=CONTINENT > ANTARCTICA > Mt Wishart&rft_subject=CONTINENT > ANTARCTICA > Mt Starlight&rft_subject=CONTINENT > ANTARCTICA > Corry Massif&rft_subject=CONTINENT > ANTARCTICA > Mt Forecast&rft_subject=CONTINENT > ANTARCTICA > Mawson Station&rft_subject=CONTINENT > ANTARCTICA > Field Rock&rft_subject=CONTINENT > ANTARCTICA > Rumdoodle&rft_subject=CONTINENT > ANTARCTICA > Bechervaise Island&rft_subject=CONTINENT > ANTARCTICA > Vestfold Hills&rft_subject=GEOGRAPHIC REGION > POLAR&rft_place=Hobart&rft.type=dataset&rft.language=English Access the data

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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_354 when using these data.

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Brief description

An analysis of bedrock and associated soils was conducted at a series of coastal localities in East Antarctica as well as further inland in the Prince Charles Mountains. Protozoans and micrometazoans were extracted from soil samples and an assessment made of their ecological relations with each other and with soil characteristics. Mineral soils, regardless of topographic elevation and proximity to the coast, were characterised by large gravel fractions (fragments of underlying bedrock) and minimal clay fractions, implying that these soils were predominantly the products of physical weathering, with little chemical alteration. Only where humans, dogs or birds contributed organic matter were there elevated concentrations of nitrogen, phosphorus or organic matter. Generally, mineral nitrogen did not seem to have resulted from microbial mineralisation, but at some sites there was evidence that atmospheric nitrate had been concentrated by sublimination of snow. Water-soluble and dilute acid-soluble phosphorous concentrations were surprisingly high for such organically poor soils. There was a sufficiently large labile pool of common macronutrients to sustain the autotrophic activity likely to occur within the bounds of prevailing temperatures and moisture; thus nutrients are not likely to be limiting for these soil communities. There was a limited fauna. Flagellates were rare and ciliates occurred only in the coastal areas sampled, whereas amoebae were found over a greater geographic and elevational span. Micrometazoans such as rotifers, tardigrades and nematodes were more common in coastal soils than in those further inland, but occurred in soils over most of the naturally occurring range of soil moistures, acidities, nutrient levels, electrolyte levels and organic contents. Exceptions were the exclusion of rotifers from alkaline soils with high nutrient levels, and the tendency of nematodes to be absent from soils with low pH. Tardigrades were found at almost all levels of soil characterisitcs. The occurrence of these metazoan phyla under such a range of environments probably resulted from their known capacity to alternate between endurance of inclement conditions in a state of deep dormancy (anhydrobiosis), and taking advantage of ephemeral favourable conditions by temporarily resuming metabolic activity. The conditions measured in soils containing micrometazoans may merely indicate thise conditions these animals can survive while dormant, not those under which active animals can carry out vital processes. In some localities there were positive associations between various taxon-pairs of metazoans and protozoans, whereas at others their occurrences seemed to be random with respect to each other. The fields for this dataset are: TARDIGRADES site AMOEBAE bedrock type quartz garnet pyroxene homblende biotite K-feldspar plagioclase Others rock type field sample number catalogue Number material USDA texture class clay mineralology water content pH KCl pH H2O micro siemens per centimetre water solution P water solution K colour (Munsell) Total N Minimum N (KCl) NH3-N Dilute acid solution P loss on ignition (%) Ciliates nematodes associations

Issued: 2000-07-27

Data time period: 1990-01-06 to 1990-02-03

This dataset is part of a larger collection

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text: northlimit=-67.5833; southlimit=-71.4166; westlimit=62.8166; eastLimit=78.0; projection=WGS84

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AU-ANL:PEAU : http://nla.gov.au/nla.party-617536 NLA Link

Identifiers

URI : data.aad.gov.au/metadata/records/ASAC_354
Local : ASAC_354
DOI : 10.4225/15/57E4AB7A4F788
global : aec1bd72-a7f3-4a62-80c8-d644d2663d21

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