Chronology, dose rates, and stable isotope record of sediment core MD03-2607
Reconstructions of primary productivity at low latitudes have been the focus of several studies to better understand how the export of nutrient-rich, intermediate Southern Ocean (SO) waters influences productivity at these latitudes. This was triggered by the general observation of minima in the pla...
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ftpangaea:oai:pangaea.de:doi:10.1594/PANGAEA.878135 2023-05-15T18:25:42+02:00 Chronology, dose rates, and stable isotope record of sediment core MD03-2607 Lopes dos Santos, Raquel A Wilkins, Michael J De Deckker, Patrick Schouten, Stefan LATITUDE: -36.960700 * LONGITUDE: 137.406500 * DATE/TIME START: 2003-02-20T19:33:00 * DATE/TIME END: 2003-02-20T19:33:00 2012-07-25 application/zip, 2 datasets https://doi.pangaea.de/10.1594/PANGAEA.878135 https://doi.org/10.1594/PANGAEA.878135 en eng PANGAEA https://doi.pangaea.de/10.1594/PANGAEA.878135 https://doi.org/10.1594/PANGAEA.878135 CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess CC-BY Supplement to: Lopes dos Santos, Raquel A; Wilkins, Michael J; De Deckker, Patrick; Schouten, Stefan (2012): Late Quaternary productivity changes from offshore Southeastern Australia: A biomarker approach. Palaeogeography, Palaeoclimatology, Palaeoecology, 363-364, 48-56, https://doi.org/10.1016/j.palaeo.2012.08.013 NIOZ_UU NIOZ Royal Netherlands Institute for Sea Research and Utrecht University Dataset 2012 ftpangaea https://doi.org/10.1594/PANGAEA.878135 https://doi.org/10.1016/j.palaeo.2012.08.013 2023-01-20T07:33:59Z Reconstructions of primary productivity at low latitudes have been the focus of several studies to better understand how the export of nutrient-rich, intermediate Southern Ocean (SO) waters influences productivity at these latitudes. This was triggered by the general observation of minima in the planktonic foraminiferal d13C values during deglaciations, which was interpreted as an isotopic signal of intermediate SO waters, together with concomitant increase in diatom productivity at some equatorial sites. However, the impact of these SO waters on productivity at higher latitudes is not well constrained. Here, we compare a high-resolution planktonic foraminiferal d13C record with total organic carbon and biomarker records for Proboscia diatoms and haptophytes from a core offshore Southeastern Australia (SEA). This shows that SEA received intermediate SO waters during deglaciations but it did not result in increased productivity during these periods. Instead, the highest primary productivity period, as shown by total organic carbon and alkenone accumulation rates, was during Last Glacial Maximum while Proboscia diatoms mainly proliferated during interglacials and Marine Isotope Stage 3, matching periods of increased diatom productivity in some sites of the Eastern Equatorial Pacific. Our study suggests that increased primary productivity offshore SEA is mainly due to stronger westerlies winds during glacial while Proboscia diatom productivity is likely to be also controlled by the transport of silicic acid to this area. Dataset Southern Ocean PANGAEA - Data Publisher for Earth & Environmental Science Southern Ocean Pacific ENVELOPE(137.406500,137.406500,-36.960700,-36.960700) |
institution |
Open Polar |
collection |
PANGAEA - Data Publisher for Earth & Environmental Science |
op_collection_id |
ftpangaea |
language |
English |
topic |
NIOZ_UU NIOZ Royal Netherlands Institute for Sea Research and Utrecht University |
spellingShingle |
NIOZ_UU NIOZ Royal Netherlands Institute for Sea Research and Utrecht University Lopes dos Santos, Raquel A Wilkins, Michael J De Deckker, Patrick Schouten, Stefan Chronology, dose rates, and stable isotope record of sediment core MD03-2607 |
topic_facet |
NIOZ_UU NIOZ Royal Netherlands Institute for Sea Research and Utrecht University |
description |
Reconstructions of primary productivity at low latitudes have been the focus of several studies to better understand how the export of nutrient-rich, intermediate Southern Ocean (SO) waters influences productivity at these latitudes. This was triggered by the general observation of minima in the planktonic foraminiferal d13C values during deglaciations, which was interpreted as an isotopic signal of intermediate SO waters, together with concomitant increase in diatom productivity at some equatorial sites. However, the impact of these SO waters on productivity at higher latitudes is not well constrained. Here, we compare a high-resolution planktonic foraminiferal d13C record with total organic carbon and biomarker records for Proboscia diatoms and haptophytes from a core offshore Southeastern Australia (SEA). This shows that SEA received intermediate SO waters during deglaciations but it did not result in increased productivity during these periods. Instead, the highest primary productivity period, as shown by total organic carbon and alkenone accumulation rates, was during Last Glacial Maximum while Proboscia diatoms mainly proliferated during interglacials and Marine Isotope Stage 3, matching periods of increased diatom productivity in some sites of the Eastern Equatorial Pacific. Our study suggests that increased primary productivity offshore SEA is mainly due to stronger westerlies winds during glacial while Proboscia diatom productivity is likely to be also controlled by the transport of silicic acid to this area. |
format |
Dataset |
author |
Lopes dos Santos, Raquel A Wilkins, Michael J De Deckker, Patrick Schouten, Stefan |
author_facet |
Lopes dos Santos, Raquel A Wilkins, Michael J De Deckker, Patrick Schouten, Stefan |
author_sort |
Lopes dos Santos, Raquel A |
title |
Chronology, dose rates, and stable isotope record of sediment core MD03-2607 |
title_short |
Chronology, dose rates, and stable isotope record of sediment core MD03-2607 |
title_full |
Chronology, dose rates, and stable isotope record of sediment core MD03-2607 |
title_fullStr |
Chronology, dose rates, and stable isotope record of sediment core MD03-2607 |
title_full_unstemmed |
Chronology, dose rates, and stable isotope record of sediment core MD03-2607 |
title_sort |
chronology, dose rates, and stable isotope record of sediment core md03-2607 |
publisher |
PANGAEA |
publishDate |
2012 |
url |
https://doi.pangaea.de/10.1594/PANGAEA.878135 https://doi.org/10.1594/PANGAEA.878135 |
op_coverage |
LATITUDE: -36.960700 * LONGITUDE: 137.406500 * DATE/TIME START: 2003-02-20T19:33:00 * DATE/TIME END: 2003-02-20T19:33:00 |
long_lat |
ENVELOPE(137.406500,137.406500,-36.960700,-36.960700) |
geographic |
Southern Ocean Pacific |
geographic_facet |
Southern Ocean Pacific |
genre |
Southern Ocean |
genre_facet |
Southern Ocean |
op_source |
Supplement to: Lopes dos Santos, Raquel A; Wilkins, Michael J; De Deckker, Patrick; Schouten, Stefan (2012): Late Quaternary productivity changes from offshore Southeastern Australia: A biomarker approach. Palaeogeography, Palaeoclimatology, Palaeoecology, 363-364, 48-56, https://doi.org/10.1016/j.palaeo.2012.08.013 |
op_relation |
https://doi.pangaea.de/10.1594/PANGAEA.878135 https://doi.org/10.1594/PANGAEA.878135 |
op_rights |
CC-BY-3.0: Creative Commons Attribution 3.0 Unported Access constraints: unrestricted info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1594/PANGAEA.878135 https://doi.org/10.1016/j.palaeo.2012.08.013 |
_version_ |
1766207308279316480 |