SWATT leaf d13C
Isotope ratio mass spectrometry (IRMS): Leaf tissue samples from were dried in synthetic gauze bags on silica gel. Samples from species that occurred at more than seven sites (see Table SWATT_climate2.csv for locations) were selected, with the exception of one species (Grevillea hookeriana), which i...
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Terrestrial Ecosystem Research Network
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Online Access: | https://researchdata.edu.au/swatt-leaf-d13c/2048042 https://geonetwork.tern.org.au/geonetwork/srv/eng/catalog.search#/metadata/6564a202-6665-4a48-b72d-2c3b10f0fd48 |
id |
ftands:oai:ands.org.au::2048042 |
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record_format |
openpolar |
institution |
Open Polar |
collection |
Research Data Australia (Australian National Data Service - ANDS) |
op_collection_id |
ftands |
language |
unknown |
topic |
biota CARBON ISOTOPE EARTH SCIENCE CLIMATE INDICATORS PALEOCLIMATE INDICATORS BIOLOGICAL RECORDS TREE RINGS ISOTOPIC ANALYSIS NITROGEN ISOTOPES ICE CORE RECORDS ISOTOPES STABLE ISOTOPES DROUGHTS HUMAN DIMENSIONS NATURAL HAZARDS TERRESTRIAL ECOSYSTEMS BIOSPHERE Climate change science Ecological impacts of climate change and ecological adaptation field species name (Unitless) Unitless leaf carbon content (Percent) Percent mean leaf nitrogen content (Percent) maximum temperature (Degree Celsius) Degree Celsius elevation of site (Metre) Metre growth form (Unitless) leaf Delta13C (Parts per thousand) Parts per thousand leaf Delta15N (Parts per thousand) 250 km - < 500 km or approximately 2.5 degrees - < 5.0 degrees irregular Arid ecology Ecosystem Modelling Long-Term Community Monitoring Long-Term Species Monitoring leaf isotopes Climate Landscape Type Native Vegetation Vegetation Structure |
spellingShingle |
biota CARBON ISOTOPE EARTH SCIENCE CLIMATE INDICATORS PALEOCLIMATE INDICATORS BIOLOGICAL RECORDS TREE RINGS ISOTOPIC ANALYSIS NITROGEN ISOTOPES ICE CORE RECORDS ISOTOPES STABLE ISOTOPES DROUGHTS HUMAN DIMENSIONS NATURAL HAZARDS TERRESTRIAL ECOSYSTEMS BIOSPHERE Climate change science Ecological impacts of climate change and ecological adaptation field species name (Unitless) Unitless leaf carbon content (Percent) Percent mean leaf nitrogen content (Percent) maximum temperature (Degree Celsius) Degree Celsius elevation of site (Metre) Metre growth form (Unitless) leaf Delta13C (Parts per thousand) Parts per thousand leaf Delta15N (Parts per thousand) 250 km - < 500 km or approximately 2.5 degrees - < 5.0 degrees irregular Arid ecology Ecosystem Modelling Long-Term Community Monitoring Long-Term Species Monitoring leaf isotopes Climate Landscape Type Native Vegetation Vegetation Structure SWATT leaf d13C |
topic_facet |
biota CARBON ISOTOPE EARTH SCIENCE CLIMATE INDICATORS PALEOCLIMATE INDICATORS BIOLOGICAL RECORDS TREE RINGS ISOTOPIC ANALYSIS NITROGEN ISOTOPES ICE CORE RECORDS ISOTOPES STABLE ISOTOPES DROUGHTS HUMAN DIMENSIONS NATURAL HAZARDS TERRESTRIAL ECOSYSTEMS BIOSPHERE Climate change science Ecological impacts of climate change and ecological adaptation field species name (Unitless) Unitless leaf carbon content (Percent) Percent mean leaf nitrogen content (Percent) maximum temperature (Degree Celsius) Degree Celsius elevation of site (Metre) Metre growth form (Unitless) leaf Delta13C (Parts per thousand) Parts per thousand leaf Delta15N (Parts per thousand) 250 km - < 500 km or approximately 2.5 degrees - < 5.0 degrees irregular Arid ecology Ecosystem Modelling Long-Term Community Monitoring Long-Term Species Monitoring leaf isotopes Climate Landscape Type Native Vegetation Vegetation Structure |
description |
Isotope ratio mass spectrometry (IRMS): Leaf tissue samples from were dried in synthetic gauze bags on silica gel. Samples from species that occurred at more than seven sites (see Table SWATT_climate2.csv for locations) were selected, with the exception of one species (Grevillea hookeriana), which is only present at six sites. Leaves were ground using a ball mill (Retsch MM400 fitted with a Qiagen TissueLyser 24 adapter set). Leaves that did not grind within 3 minutes in the TissueLyzer (for example, Allocasuarina spinosissima) were ground in a 5 mL stainless steel grinding jar. For carbon and nitrogen isotope analysis, 2-2.5 mg of ground material was weighed to six significant figures into a tin capsule using an A&D BM-22 microbalance. Technical replicates for 13% of samples were run to correct for drift. Samples were combusted at 1000°C in an Elemental Analyser (EuroVector EuroEA 3000) in line with a continuous flow isotope ratio mass spectrometer (Nu Instruments Nu Horizon, University of Adelaide). Pure glycine, glutamic acid and triphenylamine (all calibrated to international C & N standards) were used as standards. A standard error of 0.07‰ was achieved. Two-point drift and size corrections based on glycine and glutamic acid standards were undertaken. Growth forms were attributed to species based on the growth forms described in the National Vegetation Attribute Manual (ESCAVI, 2003) with grasses and forbs further divided in to annual and perennial groups. Sub-specific determinations were ignored. Climate data were extracted from BIOCLIM layers modelled at 9 second resolution extracted from ANUCLIM 6.1 (Xu & Hutchinson, 2013). Credit We at TERN acknowledge the Traditional Owners and Custodians throughout Australia, New Zealand and all nations. We honour their profound connections to land, water, biodiversity and culture and pay our respects to their Elders past, present and emerging. Purpose This project was established to investigate the leaf stable carbon isotope response of terrestrial ... |
author2 |
Byrne, Margaret (coAuthor) Caddy-Retalic, Stefan (author) Curtin University (hasAssociationWith) Department of Biodiversity, Conservation and Attractions, Western Australian Government (hasAssociationWith) McInerney, Francesca (coAuthor) Nielson, Kristine (pointOfContact) Nielson, Kristine (coAuthor) Terrestrial Ecosystem Research Network (distributor) Terrestrial Ecosystem Research Network (publisher) Terrestrial Ecosystem Research Network (pointOfContact) University of Adelaide (hasAssociationWith) van Leeuwen, Stephen (coAuthor) |
format |
Dataset |
title |
SWATT leaf d13C |
title_short |
SWATT leaf d13C |
title_full |
SWATT leaf d13C |
title_fullStr |
SWATT leaf d13C |
title_full_unstemmed |
SWATT leaf d13C |
title_sort |
swatt leaf d13c |
publisher |
Terrestrial Ecosystem Research Network |
url |
https://researchdata.edu.au/swatt-leaf-d13c/2048042 https://geonetwork.tern.org.au/geonetwork/srv/eng/catalog.search#/metadata/6564a202-6665-4a48-b72d-2c3b10f0fd48 |
op_coverage |
Spatial: South Wet Australian Transect (SWAT)- 27 sites spanning 9.56 degrees latitude and 6.85 degrees longitude. IBRA region: Avon Wheatbelt; Coolgardie ;Esperance Plains; Great Victoria Desert; Jarrah Forest; Little Sandy Desert; Mallee; Murchison; Swan Coastal Plain Spatial: northlimit=-25.05675; southlimit=-34.61918; westlimit=116.75; eastLimit=123.59623; projection=EPSG:3577 Temporal: From 1983-11-04 to 2016-10-12 |
long_lat |
ENVELOPE(144.250,144.250,-67.317,-67.317) ENVELOPE(116.75,123.59623,-25.05675,-34.61918) |
geographic |
New Zealand Murchison |
geographic_facet |
New Zealand Murchison |
genre |
ice core |
genre_facet |
ice core |
op_source |
University of Adelaide |
op_relation |
https://researchdata.edu.au/swatt-leaf-d13c/2048042 6564a202-6665-4a48-b72d-2c3b10f0fd48 https://geonetwork.tern.org.au/geonetwork/srv/eng/catalog.search#/metadata/6564a202-6665-4a48-b72d-2c3b10f0fd48 |
_version_ |
1778526673513218048 |
spelling |
ftands:oai:ands.org.au::2048042 2023-10-01T03:56:39+02:00 SWATT leaf d13C Byrne, Margaret (coAuthor) Caddy-Retalic, Stefan (author) Curtin University (hasAssociationWith) Department of Biodiversity, Conservation and Attractions, Western Australian Government (hasAssociationWith) McInerney, Francesca (coAuthor) Nielson, Kristine (pointOfContact) Nielson, Kristine (coAuthor) Terrestrial Ecosystem Research Network (distributor) Terrestrial Ecosystem Research Network (publisher) Terrestrial Ecosystem Research Network (pointOfContact) University of Adelaide (hasAssociationWith) van Leeuwen, Stephen (coAuthor) Spatial: South Wet Australian Transect (SWAT)- 27 sites spanning 9.56 degrees latitude and 6.85 degrees longitude. IBRA region: Avon Wheatbelt; Coolgardie ;Esperance Plains; Great Victoria Desert; Jarrah Forest; Little Sandy Desert; Mallee; Murchison; Swan Coastal Plain Spatial: northlimit=-25.05675; southlimit=-34.61918; westlimit=116.75; eastLimit=123.59623; projection=EPSG:3577 Temporal: From 1983-11-04 to 2016-10-12 https://researchdata.edu.au/swatt-leaf-d13c/2048042 https://geonetwork.tern.org.au/geonetwork/srv/eng/catalog.search#/metadata/6564a202-6665-4a48-b72d-2c3b10f0fd48 unknown Terrestrial Ecosystem Research Network https://researchdata.edu.au/swatt-leaf-d13c/2048042 6564a202-6665-4a48-b72d-2c3b10f0fd48 https://geonetwork.tern.org.au/geonetwork/srv/eng/catalog.search#/metadata/6564a202-6665-4a48-b72d-2c3b10f0fd48 University of Adelaide biota CARBON ISOTOPE EARTH SCIENCE CLIMATE INDICATORS PALEOCLIMATE INDICATORS BIOLOGICAL RECORDS TREE RINGS ISOTOPIC ANALYSIS NITROGEN ISOTOPES ICE CORE RECORDS ISOTOPES STABLE ISOTOPES DROUGHTS HUMAN DIMENSIONS NATURAL HAZARDS TERRESTRIAL ECOSYSTEMS BIOSPHERE Climate change science Ecological impacts of climate change and ecological adaptation field species name (Unitless) Unitless leaf carbon content (Percent) Percent mean leaf nitrogen content (Percent) maximum temperature (Degree Celsius) Degree Celsius elevation of site (Metre) Metre growth form (Unitless) leaf Delta13C (Parts per thousand) Parts per thousand leaf Delta15N (Parts per thousand) 250 km - < 500 km or approximately 2.5 degrees - < 5.0 degrees irregular Arid ecology Ecosystem Modelling Long-Term Community Monitoring Long-Term Species Monitoring leaf isotopes Climate Landscape Type Native Vegetation Vegetation Structure dataset ftands 2023-09-04T22:31:37Z Isotope ratio mass spectrometry (IRMS): Leaf tissue samples from were dried in synthetic gauze bags on silica gel. Samples from species that occurred at more than seven sites (see Table SWATT_climate2.csv for locations) were selected, with the exception of one species (Grevillea hookeriana), which is only present at six sites. Leaves were ground using a ball mill (Retsch MM400 fitted with a Qiagen TissueLyser 24 adapter set). Leaves that did not grind within 3 minutes in the TissueLyzer (for example, Allocasuarina spinosissima) were ground in a 5 mL stainless steel grinding jar. For carbon and nitrogen isotope analysis, 2-2.5 mg of ground material was weighed to six significant figures into a tin capsule using an A&D BM-22 microbalance. Technical replicates for 13% of samples were run to correct for drift. Samples were combusted at 1000°C in an Elemental Analyser (EuroVector EuroEA 3000) in line with a continuous flow isotope ratio mass spectrometer (Nu Instruments Nu Horizon, University of Adelaide). Pure glycine, glutamic acid and triphenylamine (all calibrated to international C & N standards) were used as standards. A standard error of 0.07‰ was achieved. Two-point drift and size corrections based on glycine and glutamic acid standards were undertaken. Growth forms were attributed to species based on the growth forms described in the National Vegetation Attribute Manual (ESCAVI, 2003) with grasses and forbs further divided in to annual and perennial groups. Sub-specific determinations were ignored. Climate data were extracted from BIOCLIM layers modelled at 9 second resolution extracted from ANUCLIM 6.1 (Xu & Hutchinson, 2013). Credit We at TERN acknowledge the Traditional Owners and Custodians throughout Australia, New Zealand and all nations. We honour their profound connections to land, water, biodiversity and culture and pay our respects to their Elders past, present and emerging. Purpose This project was established to investigate the leaf stable carbon isotope response of terrestrial ... Dataset ice core Research Data Australia (Australian National Data Service - ANDS) New Zealand Murchison ENVELOPE(144.250,144.250,-67.317,-67.317) ENVELOPE(116.75,123.59623,-25.05675,-34.61918) |