Antarctic diatom silicification diminishes under ocean acidification

No problems were encountered with data collection. The six level fCO2 gradient approach meant that our data could be analysed using a regression model, allowing us to identify functional relationships between our fCO2 treatment and our response variables. Gradient designs are more effective at uncov...

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Bibliographic Details
Other Authors: AADC (originator), AU/AADC > Australian Antarctic Data Centre, Australia (resourceProvider)
Format: Dataset
Language:unknown
Published: Australian Ocean Data Network
Subjects:
AMD
Online Access:https://researchdata.ands.org.au/antarctic-diatom-silicification-ocean-acidification/1361086
https://data.aad.gov.au/metadata/records/AAS_4026_Silicification_CO2
https://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4026_Silicification_CO2
https://secure3.aad.gov.au/proms/public/projects/report_project_public.cfm?project_no=AAS_4026
https://data.aad.gov.au/eds/4840/download
id ftands:oai:ands.org.au::1361086
record_format openpolar
institution Open Polar
collection Research Data Australia (Australian National Data Service - ANDS)
op_collection_id ftands
language unknown
topic biota
environment
oceans
DIATOMS
EARTH SCIENCE
BIOLOGICAL CLASSIFICATION
PLANTS
MICROALGAE
SILICATE
OCEAN CHEMISTRY
CARBON CYCLE/CARBON BUDGET MODELS
EARTH SCIENCE SERVICES
MODELS
SILICIFICATION
CARBON CYCLING
OCEAN ACIDIFICATION
MESOCOSM
MINICOSM
SPECTROPHOTOMETERS
PAM &gt
PORTABLE FLUORESCENCE ANALYZERS
FLUOROMETERS
FLUORESCENCE MICROSCOPY
FIELD INVESTIGATION
FIELD SURVEYS
LABORATORY
AMD/AU
AMD
CEOS
GEOGRAPHIC REGION &gt
POLAR
CONTINENT &gt
ANTARCTICA &gt
DAVIS STATION
OCEAN &gt
SOUTHERN OCEAN &gt
PRYDZ BAY
spellingShingle biota
environment
oceans
DIATOMS
EARTH SCIENCE
BIOLOGICAL CLASSIFICATION
PLANTS
MICROALGAE
SILICATE
OCEAN CHEMISTRY
CARBON CYCLE/CARBON BUDGET MODELS
EARTH SCIENCE SERVICES
MODELS
SILICIFICATION
CARBON CYCLING
OCEAN ACIDIFICATION
MESOCOSM
MINICOSM
SPECTROPHOTOMETERS
PAM &gt
PORTABLE FLUORESCENCE ANALYZERS
FLUOROMETERS
FLUORESCENCE MICROSCOPY
FIELD INVESTIGATION
FIELD SURVEYS
LABORATORY
AMD/AU
AMD
CEOS
GEOGRAPHIC REGION &gt
POLAR
CONTINENT &gt
ANTARCTICA &gt
DAVIS STATION
OCEAN &gt
SOUTHERN OCEAN &gt
PRYDZ BAY
Antarctic diatom silicification diminishes under ocean acidification
topic_facet biota
environment
oceans
DIATOMS
EARTH SCIENCE
BIOLOGICAL CLASSIFICATION
PLANTS
MICROALGAE
SILICATE
OCEAN CHEMISTRY
CARBON CYCLE/CARBON BUDGET MODELS
EARTH SCIENCE SERVICES
MODELS
SILICIFICATION
CARBON CYCLING
OCEAN ACIDIFICATION
MESOCOSM
MINICOSM
SPECTROPHOTOMETERS
PAM &gt
PORTABLE FLUORESCENCE ANALYZERS
FLUOROMETERS
FLUORESCENCE MICROSCOPY
FIELD INVESTIGATION
FIELD SURVEYS
LABORATORY
AMD/AU
AMD
CEOS
GEOGRAPHIC REGION &gt
POLAR
CONTINENT &gt
ANTARCTICA &gt
DAVIS STATION
OCEAN &gt
SOUTHERN OCEAN &gt
PRYDZ BAY
description No problems were encountered with data collection. The six level fCO2 gradient approach meant that our data could be analysed using a regression model, allowing us to identify functional relationships between our fCO2 treatment and our response variables. Gradient designs are more effective at uncovering underlying responses patterns to environmental drivers, improving interpolation potential and generally deliver more useful quantitative information for models. This data set was collected during an ocean acidification mesocosm experiment performed at Davis Station, Antarctica during the 2014/15 summer season. It includes: - description of methods for all data collection and analyses. - diatom cell volume - bulk silicification - species specific silicification via fluorescence microscopy - bulk community Fv/Fm on day 12 - single-cell PAM fluorometry data (maximum quantum yield of PSII: Fv/Fm) A natural community of Antarctic marine microbes from Prydz Bay, East Antarctica were exposed to a range of CO2 concentrations in 650 L minicosms to simulate possible future ocean conditions up to the year ~2200. Diatom silica precipitation rates were examined at CO2 concentrations between 343 to 1641 micro atm, measuring both the total diatom community response and that of individual species, to determine whether ocean acidification may influence future diatom ballast and therefore alter carbon and silica fluxes in the Southern Ocean. Described and analysed in: Antarctic diatom silicification diminishes under ocean acidification (submitted for review) Methods described in: Antarctic diatom silicification diminishes under ocean acidification (submitted for review) Location: Prydz bay, Davis Station, Antarctica (68 degrees 35'S, 77 degrees 58' E) Date: Summer 2014/2015 Worksheet descriptions: Bulk silicification - raw data Measured total and incorporated biogenic silica using spectrophotometer for all tanks on day 12 after 24 h incubation with PDMPO - raw data Bulk Fv/Fm - dark-adapted maximum quantum efficiency of PSII (Fv/Fm) on whole community - raw data Measured Fv/Fm of individual cells from 3 mesocosm tanks. Single-cell silicificiation, Fluorescence microscopy - raw data Measured autofluorescence and PDMPO fluorescence of individual diatoms from 6 mesocosm tanks Single-cell PAM, dark-adapted maximum quantum efficiency of PSII (Fv/Fm) - raw data Measured Fv/Fm of individual cells from 3 mesocosm tanks. Cell volume Calculated cell volume (um3) of 7 species from minicosm tanks 1 and 6 - raw data Abbreviations: Fv/Fm Maximum quantum yield of PSII PDMPO 2-(4-pyridyl)-5-((4-(2-dimethylaminoethylaminocarbamoyl)methoxy)phenyl)oxazole Tant Thalassiosira antarctica DiscLg Large Discoid centric diatoms Stella Stellarima microtrias Chaeto Chaetoceros spp. Prob Proboscia truncata Pseu Pseudonitzschia turgiduloides FragLg Fragilariopsis cylindrus / curta Centric Large Discoid centric diatoms LargeThalassiosira Large Discoid centric diatoms Based on the results of a previous study, a natural community of Antarctic marine microbes from Prydz Bay, East Antarctica were exposed to a range of CO2 concentrations in 650 L mesocosms to simulate possible future ocean conditions up to the year ∼2200. Diatom silica precipitation rates were examined at CO2 concentrations between 343 to 1641 micro atm, measuring both the total diatom community response and that of individual species, to determine whether ocean acidification may influence future diatom ballast and therefore alter carbon and silica fluxes in the Southern Ocean.
author2 AADC (originator)
AU/AADC > Australian Antarctic Data Centre, Australia (resourceProvider)
format Dataset
title Antarctic diatom silicification diminishes under ocean acidification
title_short Antarctic diatom silicification diminishes under ocean acidification
title_full Antarctic diatom silicification diminishes under ocean acidification
title_fullStr Antarctic diatom silicification diminishes under ocean acidification
title_full_unstemmed Antarctic diatom silicification diminishes under ocean acidification
title_sort antarctic diatom silicification diminishes under ocean acidification
publisher Australian Ocean Data Network
url https://researchdata.ands.org.au/antarctic-diatom-silicification-ocean-acidification/1361086
https://data.aad.gov.au/metadata/records/AAS_4026_Silicification_CO2
https://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4026_Silicification_CO2
https://secure3.aad.gov.au/proms/public/projects/report_project_public.cfm?project_no=AAS_4026
https://data.aad.gov.au/eds/4840/download
op_coverage Spatial: northlimit=-67.38509; southlimit=-69.79988; westlimit=73.75; eastLimit=82.69531
Temporal: From 2014-11-19 to 2015-01-14
long_lat ENVELOPE(77.968,77.968,-68.576,-68.576)
ENVELOPE(77.968,77.968,-68.576,-68.576)
ENVELOPE(-64.254,-64.254,-65.249,-65.249)
ENVELOPE(73.75,82.69531,-67.38509,-69.79988)
geographic Antarctic
Davis Station
Davis-Station
East Antarctica
Prydz Bay
Southern Ocean
Stella
geographic_facet Antarctic
Davis Station
Davis-Station
East Antarctica
Prydz Bay
Southern Ocean
Stella
genre Antarc*
Antarctic
Antarctica
East Antarctica
Ocean acidification
Prydz Bay
Southern Ocean
genre_facet Antarc*
Antarctic
Antarctica
East Antarctica
Ocean acidification
Prydz Bay
Southern Ocean
op_source https://data.aad.gov.au
op_relation https://researchdata.ands.org.au/antarctic-diatom-silicification-ocean-acidification/1361086
e47966c2-12c0-4f85-b96a-85803469ddd0
https://data.aad.gov.au/metadata/records/AAS_4026_Silicification_CO2
https://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4026_Silicification_CO2
https://secure3.aad.gov.au/proms/public/projects/report_project_public.cfm?project_no=AAS_4026
https://data.aad.gov.au/eds/4840/download
_version_ 1766247718823395328
spelling ftands:oai:ands.org.au::1361086 2023-05-15T13:47:42+02:00 Antarctic diatom silicification diminishes under ocean acidification AADC (originator) AU/AADC > Australian Antarctic Data Centre, Australia (resourceProvider) Spatial: northlimit=-67.38509; southlimit=-69.79988; westlimit=73.75; eastLimit=82.69531 Temporal: From 2014-11-19 to 2015-01-14 https://researchdata.ands.org.au/antarctic-diatom-silicification-ocean-acidification/1361086 https://data.aad.gov.au/metadata/records/AAS_4026_Silicification_CO2 https://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4026_Silicification_CO2 https://secure3.aad.gov.au/proms/public/projects/report_project_public.cfm?project_no=AAS_4026 https://data.aad.gov.au/eds/4840/download unknown Australian Ocean Data Network https://researchdata.ands.org.au/antarctic-diatom-silicification-ocean-acidification/1361086 e47966c2-12c0-4f85-b96a-85803469ddd0 https://data.aad.gov.au/metadata/records/AAS_4026_Silicification_CO2 https://data.aad.gov.au/aadc/metadata/citation.cfm?entry_id=AAS_4026_Silicification_CO2 https://secure3.aad.gov.au/proms/public/projects/report_project_public.cfm?project_no=AAS_4026 https://data.aad.gov.au/eds/4840/download https://data.aad.gov.au biota environment oceans DIATOMS EARTH SCIENCE BIOLOGICAL CLASSIFICATION PLANTS MICROALGAE SILICATE OCEAN CHEMISTRY CARBON CYCLE/CARBON BUDGET MODELS EARTH SCIENCE SERVICES MODELS SILICIFICATION CARBON CYCLING OCEAN ACIDIFICATION MESOCOSM MINICOSM SPECTROPHOTOMETERS PAM &gt PORTABLE FLUORESCENCE ANALYZERS FLUOROMETERS FLUORESCENCE MICROSCOPY FIELD INVESTIGATION FIELD SURVEYS LABORATORY AMD/AU AMD CEOS GEOGRAPHIC REGION &gt POLAR CONTINENT &gt ANTARCTICA &gt DAVIS STATION OCEAN &gt SOUTHERN OCEAN &gt PRYDZ BAY dataset ftands 2020-01-05T22:23:21Z No problems were encountered with data collection. The six level fCO2 gradient approach meant that our data could be analysed using a regression model, allowing us to identify functional relationships between our fCO2 treatment and our response variables. Gradient designs are more effective at uncovering underlying responses patterns to environmental drivers, improving interpolation potential and generally deliver more useful quantitative information for models. This data set was collected during an ocean acidification mesocosm experiment performed at Davis Station, Antarctica during the 2014/15 summer season. It includes: - description of methods for all data collection and analyses. - diatom cell volume - bulk silicification - species specific silicification via fluorescence microscopy - bulk community Fv/Fm on day 12 - single-cell PAM fluorometry data (maximum quantum yield of PSII: Fv/Fm) A natural community of Antarctic marine microbes from Prydz Bay, East Antarctica were exposed to a range of CO2 concentrations in 650 L minicosms to simulate possible future ocean conditions up to the year ~2200. Diatom silica precipitation rates were examined at CO2 concentrations between 343 to 1641 micro atm, measuring both the total diatom community response and that of individual species, to determine whether ocean acidification may influence future diatom ballast and therefore alter carbon and silica fluxes in the Southern Ocean. Described and analysed in: Antarctic diatom silicification diminishes under ocean acidification (submitted for review) Methods described in: Antarctic diatom silicification diminishes under ocean acidification (submitted for review) Location: Prydz bay, Davis Station, Antarctica (68 degrees 35'S, 77 degrees 58' E) Date: Summer 2014/2015 Worksheet descriptions: Bulk silicification - raw data Measured total and incorporated biogenic silica using spectrophotometer for all tanks on day 12 after 24 h incubation with PDMPO - raw data Bulk Fv/Fm - dark-adapted maximum quantum efficiency of PSII (Fv/Fm) on whole community - raw data Measured Fv/Fm of individual cells from 3 mesocosm tanks. Single-cell silicificiation, Fluorescence microscopy - raw data Measured autofluorescence and PDMPO fluorescence of individual diatoms from 6 mesocosm tanks Single-cell PAM, dark-adapted maximum quantum efficiency of PSII (Fv/Fm) - raw data Measured Fv/Fm of individual cells from 3 mesocosm tanks. Cell volume Calculated cell volume (um3) of 7 species from minicosm tanks 1 and 6 - raw data Abbreviations: Fv/Fm Maximum quantum yield of PSII PDMPO 2-(4-pyridyl)-5-((4-(2-dimethylaminoethylaminocarbamoyl)methoxy)phenyl)oxazole Tant Thalassiosira antarctica DiscLg Large Discoid centric diatoms Stella Stellarima microtrias Chaeto Chaetoceros spp. Prob Proboscia truncata Pseu Pseudonitzschia turgiduloides FragLg Fragilariopsis cylindrus / curta Centric Large Discoid centric diatoms LargeThalassiosira Large Discoid centric diatoms Based on the results of a previous study, a natural community of Antarctic marine microbes from Prydz Bay, East Antarctica were exposed to a range of CO2 concentrations in 650 L mesocosms to simulate possible future ocean conditions up to the year ∼2200. Diatom silica precipitation rates were examined at CO2 concentrations between 343 to 1641 micro atm, measuring both the total diatom community response and that of individual species, to determine whether ocean acidification may influence future diatom ballast and therefore alter carbon and silica fluxes in the Southern Ocean. Dataset Antarc* Antarctic Antarctica East Antarctica Ocean acidification Prydz Bay Southern Ocean Research Data Australia (Australian National Data Service - ANDS) Antarctic Davis Station ENVELOPE(77.968,77.968,-68.576,-68.576) Davis-Station ENVELOPE(77.968,77.968,-68.576,-68.576) East Antarctica Prydz Bay Southern Ocean Stella ENVELOPE(-64.254,-64.254,-65.249,-65.249) ENVELOPE(73.75,82.69531,-67.38509,-69.79988)