Metadata details
AAS_4061_MD972106_data_NGEO
All scientific data collected by the Australian Antarctic program (AAp) are eventually described in the Catalogue of Australian Antarctic and Subantarctic Metadata (CAASM). CAASM can be used to search through AAp data descriptions, and it also provides links to access publicly available datasets, which can either be immediately downloaded or obtained from the Australian Antarctic Data Centre (AADC).
- Citation
- Moy, A. (2019) Varied contribution of the Southern Ocean to deglacial atmospheric CO2 rise, Ver. 1, Australian Antarctic Data Centre - doi:10.26179/5d5df822acf6c, Accessed: 2026-07-25
- Title
- Varied contribution of the Southern Ocean to deglacial atmospheric CO2 rise
- Data Centre
- Australian Antarctic Data Centre, Australia
- DOI
- doi:10.26179/5d5df822acf6c
- Created Date
- 2019-08-22
- Revision Date
- 2025-09-16
- Parent record
- None
Datasets and documents
Related links
Description
Here we use oxygen, carbon and boron isotopes, and planktonic foraminiferal shell weights in planktonic foraminifera and an alkenone-based proxy of temperature to reconstruct seawater pH and CO2 partial pressure in sub-Antarctic surface waters south of Tasmania over the past 25,000 years
Glacial–interglacial changes in atmospheric CO2 are generally attributed to changes in seawater carbon chemistry in response to large-scale shifts in the ocean’s biogeochemistry and general circulation. The Southern Ocean currently takes up more CO2 than any other and it is likely to have played a crucial role in regulating past atmospheric CO2. However, the physical, biological and chemical variables that control ocean–atmosphere CO2 exchange during glacial–interglacial cycles are not completely understood. Here we use boron isotopes and carbon isotopes in planktonic foraminifera and an alkenone-based proxy of temperature to reconstruct the seawater pH and CO2 partial pressure in sub-Antarctic surface waters south of Tasmania over the past 25,000 years, and investigate the mechanisms that regulate seawater CO2. The new record shows that surface waters in this region were a sink for atmospheric CO2 during the Last Glacial Maximum. Our reconstruction suggests changes in the strength of the biological pump and the release of deep-ocean CO2 to surface waters contributed to the last deglacial rise in atmospheric CO2. These findings demonstrate that variations in upwelling intensity and the distribution of Southern Ocean water masses in this sector played a key role in regulating atmospheric CO2 during the last glacial–interglacial cycle.
Purpose
To reconstruct seawater pH and CO2 partial pressure in sub-Antarctic surface waters, and investigate the mechanisms regulating surface water CO2 over the last glacial-interglacial cycle.
Access
These data are publicly available for download from the provided URL. For more information (including figures), please see the referenced paper.
Temporal Coverages
- Start date: 2012-07-01 - Stop date: 2018-06-30
Spatial Coverages
Science Keywords
- EARTH SCIENCE > CLIMATE INDICATORS > PALEOCLIMATE INDICATORS > OCEAN/LAKE RECORDS > OXYGEN ISOTOPES
- EARTH SCIENCE > CLIMATE INDICATORS > PALEOCLIMATE INDICATORS > OCEAN/LAKE RECORDS > ISOTOPES
- EARTH SCIENCE > CLIMATE INDICATORS > PALEOCLIMATE INDICATORS > OCEAN/LAKE RECORDS > MICROFOSSILS
- EARTH SCIENCE > BIOLOGICAL CLASSIFICATION > PROTISTS > AMOEBOIDS > FORAMINIFERS
Additional Keywords
- CARBON ISOTOPES
- BORON ISOTOPES
- FORAMINIFERAL SHELL WEIGHTS
- ALKENONE SST ESTIMATES
Locations
- GEOGRAPHIC REGION > POLAR
- OCEAN > SOUTHERN OCEAN > SOUTH TASMAN RISE
Platforms
- LABORATORY
Instruments
- ISOTOPIC RATIO MASS SPECTROMETER
Researchers
- moy, andrew (INVESTIGATOR,TECHNICAL CONTACT,DIF AUTHOR)
Use Constraints
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=AAS_4061_MD972106_data_NGEO when using these data.
