Plio-Pleistocene Perth Basin water temperatures and Leeuwin Current dynamics (Indian Ocean) derived from oxygen and clumped-isotope paleothermometry
The Pliocene sedimentary record provides a window into Earth's climate dynamics under warmer-than-present boundary conditions. However, the Pliocene cannot be considered a stable warm climate that constitutes a solid baseline for middle-of-the-road future climate projections. The increasing ava...
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Copernicus Publications
2022
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Online Access: | https://doi.org/10.5194/cp-18-1231-2022 https://cp.copernicus.org/articles/18/1231/2022/cp-18-1231-2022.pdf https://doaj.org/article/e97c4972ebdf4acd899c96a224fb24c2 |
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fttriple:oai:gotriple.eu:oai:doaj.org/article:e97c4972ebdf4acd899c96a224fb24c2 2023-05-15T18:01:07+02:00 Plio-Pleistocene Perth Basin water temperatures and Leeuwin Current dynamics (Indian Ocean) derived from oxygen and clumped-isotope paleothermometry D. De Vleeschouwer M. Peral M. Marchegiano A. Füllberg N. Meinicke H. Pälike G. Auer B. Petrick C. Snoeck S. Goderis P. Claeys 2022-06-01 https://doi.org/10.5194/cp-18-1231-2022 https://cp.copernicus.org/articles/18/1231/2022/cp-18-1231-2022.pdf https://doaj.org/article/e97c4972ebdf4acd899c96a224fb24c2 en eng Copernicus Publications doi:10.5194/cp-18-1231-2022 1814-9324 1814-9332 https://cp.copernicus.org/articles/18/1231/2022/cp-18-1231-2022.pdf https://doaj.org/article/e97c4972ebdf4acd899c96a224fb24c2 undefined Climate of the Past, Vol 18, Pp 1231-1253 (2022) geo anthro-bio Journal Article https://vocabularies.coar-repositories.org/resource_types/c_6501/ 2022 fttriple https://doi.org/10.5194/cp-18-1231-2022 2023-01-22T19:26:07Z The Pliocene sedimentary record provides a window into Earth's climate dynamics under warmer-than-present boundary conditions. However, the Pliocene cannot be considered a stable warm climate that constitutes a solid baseline for middle-of-the-road future climate projections. The increasing availability of time-continuous sedimentary archives (e.g., marine sediment cores) reveals complex temporal and spatial patterns of Pliocene ocean and climate variability on astronomical timescales. The Perth Basin is particularly interesting in that respect because it remains unclear if and how the Leeuwin Current sustained the comparably wet Pliocene climate in Western Australia, as well as how it influenced Southern Hemisphere paleoclimate variability. To constrain Leeuwin Current dynamics in time and space, this project obtained eight clumped-isotope Δ47 paleotemperatures and constructed a new orbitally resolved planktonic foraminifera (Trilobatus sacculifer) stable isotope record (δ18O) for the Plio-Pleistocene (4–2 Ma) interval of International Ocean Discovery Program (IODP) Site U1459. These new data complement an existing TEX86 record from the same site and similar planktonic isotope records from the Northern Carnarvon Basin (Ocean Drilling Program (ODP) Site 763 and IODP Site U1463). The comparison of TEX86 and Δ47 paleothermometers reveals that TEX86 likely reflects sea surface temperatures (SSTs) with a seasonal warm bias (23.8–28.9 ∘C), whereas T. sacculifer Δ47 calcification temperatures probably echo mixed-layer temperatures at the studied Site U1459 (18.9–23.2 ∘C). The isotopic δ18O gradient along a 19–29∘ S latitudinal transect, between 3.9 and 2.2 Ma, displays large variability, ranging between 0.5 ‰ and 2.0 ‰. We use the latitudinal δ18O gradient as a proxy for Leeuwin Current strength, with an inverse relationship between both. The new results challenge the interpretation that suggested a tectonic event in the Indonesian Throughflow as the cause for the rapid steepening of the isotopic gradient (0.9 ‰ to ... Article in Journal/Newspaper Planktonic foraminifera Unknown Indian Climate of the Past 18 5 1231 1253 |
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Open Polar |
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fttriple |
language |
English |
topic |
geo anthro-bio |
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geo anthro-bio D. De Vleeschouwer M. Peral M. Marchegiano A. Füllberg N. Meinicke H. Pälike G. Auer B. Petrick C. Snoeck S. Goderis P. Claeys Plio-Pleistocene Perth Basin water temperatures and Leeuwin Current dynamics (Indian Ocean) derived from oxygen and clumped-isotope paleothermometry |
topic_facet |
geo anthro-bio |
description |
The Pliocene sedimentary record provides a window into Earth's climate dynamics under warmer-than-present boundary conditions. However, the Pliocene cannot be considered a stable warm climate that constitutes a solid baseline for middle-of-the-road future climate projections. The increasing availability of time-continuous sedimentary archives (e.g., marine sediment cores) reveals complex temporal and spatial patterns of Pliocene ocean and climate variability on astronomical timescales. The Perth Basin is particularly interesting in that respect because it remains unclear if and how the Leeuwin Current sustained the comparably wet Pliocene climate in Western Australia, as well as how it influenced Southern Hemisphere paleoclimate variability. To constrain Leeuwin Current dynamics in time and space, this project obtained eight clumped-isotope Δ47 paleotemperatures and constructed a new orbitally resolved planktonic foraminifera (Trilobatus sacculifer) stable isotope record (δ18O) for the Plio-Pleistocene (4–2 Ma) interval of International Ocean Discovery Program (IODP) Site U1459. These new data complement an existing TEX86 record from the same site and similar planktonic isotope records from the Northern Carnarvon Basin (Ocean Drilling Program (ODP) Site 763 and IODP Site U1463). The comparison of TEX86 and Δ47 paleothermometers reveals that TEX86 likely reflects sea surface temperatures (SSTs) with a seasonal warm bias (23.8–28.9 ∘C), whereas T. sacculifer Δ47 calcification temperatures probably echo mixed-layer temperatures at the studied Site U1459 (18.9–23.2 ∘C). The isotopic δ18O gradient along a 19–29∘ S latitudinal transect, between 3.9 and 2.2 Ma, displays large variability, ranging between 0.5 ‰ and 2.0 ‰. We use the latitudinal δ18O gradient as a proxy for Leeuwin Current strength, with an inverse relationship between both. The new results challenge the interpretation that suggested a tectonic event in the Indonesian Throughflow as the cause for the rapid steepening of the isotopic gradient (0.9 ‰ to ... |
format |
Article in Journal/Newspaper |
author |
D. De Vleeschouwer M. Peral M. Marchegiano A. Füllberg N. Meinicke H. Pälike G. Auer B. Petrick C. Snoeck S. Goderis P. Claeys |
author_facet |
D. De Vleeschouwer M. Peral M. Marchegiano A. Füllberg N. Meinicke H. Pälike G. Auer B. Petrick C. Snoeck S. Goderis P. Claeys |
author_sort |
D. De Vleeschouwer |
title |
Plio-Pleistocene Perth Basin water temperatures and Leeuwin Current dynamics (Indian Ocean) derived from oxygen and clumped-isotope paleothermometry |
title_short |
Plio-Pleistocene Perth Basin water temperatures and Leeuwin Current dynamics (Indian Ocean) derived from oxygen and clumped-isotope paleothermometry |
title_full |
Plio-Pleistocene Perth Basin water temperatures and Leeuwin Current dynamics (Indian Ocean) derived from oxygen and clumped-isotope paleothermometry |
title_fullStr |
Plio-Pleistocene Perth Basin water temperatures and Leeuwin Current dynamics (Indian Ocean) derived from oxygen and clumped-isotope paleothermometry |
title_full_unstemmed |
Plio-Pleistocene Perth Basin water temperatures and Leeuwin Current dynamics (Indian Ocean) derived from oxygen and clumped-isotope paleothermometry |
title_sort |
plio-pleistocene perth basin water temperatures and leeuwin current dynamics (indian ocean) derived from oxygen and clumped-isotope paleothermometry |
publisher |
Copernicus Publications |
publishDate |
2022 |
url |
https://doi.org/10.5194/cp-18-1231-2022 https://cp.copernicus.org/articles/18/1231/2022/cp-18-1231-2022.pdf https://doaj.org/article/e97c4972ebdf4acd899c96a224fb24c2 |
geographic |
Indian |
geographic_facet |
Indian |
genre |
Planktonic foraminifera |
genre_facet |
Planktonic foraminifera |
op_source |
Climate of the Past, Vol 18, Pp 1231-1253 (2022) |
op_relation |
doi:10.5194/cp-18-1231-2022 1814-9324 1814-9332 https://cp.copernicus.org/articles/18/1231/2022/cp-18-1231-2022.pdf https://doaj.org/article/e97c4972ebdf4acd899c96a224fb24c2 |
op_rights |
undefined |
op_doi |
https://doi.org/10.5194/cp-18-1231-2022 |
container_title |
Climate of the Past |
container_volume |
18 |
container_issue |
5 |
container_start_page |
1231 |
op_container_end_page |
1253 |
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