Distinct seasonal changes and precession forcing of surface and subsurface temperatures in the mid-latitudinal North Atlantic during the onset of the Late Pliocene
The Late Pliocene marks the intensification of Northern Hemisphere Glaciation, offering a unique opportunity to study climate evolution and ice-sheet related feedback mechanisms. In this study, we present high-resolution Mg/Ca-based sea surface (SST) and subsurface temperatures (SubT) derived from f...
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ftcopernicus:oai:publications.copernicus.org:egusphere118460 2024-09-15T18:12:31+00:00 Distinct seasonal changes and precession forcing of surface and subsurface temperatures in the mid-latitudinal North Atlantic during the onset of the Late Pliocene Pang, Xiaolei Voelker, Antje Helga Luise Lu, Sihua Ding, Xuan 2024-03-07 application/pdf https://doi.org/10.5194/egusphere-2024-603 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-603/ eng eng doi:10.5194/egusphere-2024-603 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-603/ eISSN: Text 2024 ftcopernicus https://doi.org/10.5194/egusphere-2024-603 2024-08-28T05:24:15Z The Late Pliocene marks the intensification of Northern Hemisphere Glaciation, offering a unique opportunity to study climate evolution and ice-sheet related feedback mechanisms. In this study, we present high-resolution Mg/Ca-based sea surface (SST) and subsurface temperatures (SubT) derived from foraminiferal species Globigerinoides ruber and Globorotalia hirsuta , respectively, at the Integrated Ocean Drilling Project (IODP) Expedition 306 Site U1313 in the mid-latitudinal North Atlantic during the early Late Pliocene, 3.65 – 3.37 million years ago (Ma). We find distinct differences between our new G. ruber Mg/Ca-based SST record and previously published alkenone-based SST record from the same location. These discrepancies in both absolute values and variations highlight distinct seasonal influences. The G. ruber Mg/Ca-based SST data, reflecting summer temperatures, were primarily influenced by local summer insolation, showing a dominant precession cycle. Conversely, the variations in alkenone-based SST are found to be more indicative of cold season changes, despite previous interpretations of these records as reflecting annual mean temperatures. A simultaneous decline in Mg/Ca-based SST and SubT records from 3.65 to 3.5 Ma suggests a diminished poleward oceanic heat transport, implying a weakening of the North Atlantic Current. A comparison with early Pleistocene G. ruber Mg/Ca-based SST records shows a shift in the dominant climatic cycle from precession to obliquity, alongside a marked increase in amplitude, indicating an enhanced influence of obliquity cycles correlated with the expansion of Northern Hemisphere ice sheets. Text Ice Sheet north atlantic current North Atlantic Copernicus Publications: E-Journals |
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Copernicus Publications: E-Journals |
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English |
description |
The Late Pliocene marks the intensification of Northern Hemisphere Glaciation, offering a unique opportunity to study climate evolution and ice-sheet related feedback mechanisms. In this study, we present high-resolution Mg/Ca-based sea surface (SST) and subsurface temperatures (SubT) derived from foraminiferal species Globigerinoides ruber and Globorotalia hirsuta , respectively, at the Integrated Ocean Drilling Project (IODP) Expedition 306 Site U1313 in the mid-latitudinal North Atlantic during the early Late Pliocene, 3.65 – 3.37 million years ago (Ma). We find distinct differences between our new G. ruber Mg/Ca-based SST record and previously published alkenone-based SST record from the same location. These discrepancies in both absolute values and variations highlight distinct seasonal influences. The G. ruber Mg/Ca-based SST data, reflecting summer temperatures, were primarily influenced by local summer insolation, showing a dominant precession cycle. Conversely, the variations in alkenone-based SST are found to be more indicative of cold season changes, despite previous interpretations of these records as reflecting annual mean temperatures. A simultaneous decline in Mg/Ca-based SST and SubT records from 3.65 to 3.5 Ma suggests a diminished poleward oceanic heat transport, implying a weakening of the North Atlantic Current. A comparison with early Pleistocene G. ruber Mg/Ca-based SST records shows a shift in the dominant climatic cycle from precession to obliquity, alongside a marked increase in amplitude, indicating an enhanced influence of obliquity cycles correlated with the expansion of Northern Hemisphere ice sheets. |
format |
Text |
author |
Pang, Xiaolei Voelker, Antje Helga Luise Lu, Sihua Ding, Xuan |
spellingShingle |
Pang, Xiaolei Voelker, Antje Helga Luise Lu, Sihua Ding, Xuan Distinct seasonal changes and precession forcing of surface and subsurface temperatures in the mid-latitudinal North Atlantic during the onset of the Late Pliocene |
author_facet |
Pang, Xiaolei Voelker, Antje Helga Luise Lu, Sihua Ding, Xuan |
author_sort |
Pang, Xiaolei |
title |
Distinct seasonal changes and precession forcing of surface and subsurface temperatures in the mid-latitudinal North Atlantic during the onset of the Late Pliocene |
title_short |
Distinct seasonal changes and precession forcing of surface and subsurface temperatures in the mid-latitudinal North Atlantic during the onset of the Late Pliocene |
title_full |
Distinct seasonal changes and precession forcing of surface and subsurface temperatures in the mid-latitudinal North Atlantic during the onset of the Late Pliocene |
title_fullStr |
Distinct seasonal changes and precession forcing of surface and subsurface temperatures in the mid-latitudinal North Atlantic during the onset of the Late Pliocene |
title_full_unstemmed |
Distinct seasonal changes and precession forcing of surface and subsurface temperatures in the mid-latitudinal North Atlantic during the onset of the Late Pliocene |
title_sort |
distinct seasonal changes and precession forcing of surface and subsurface temperatures in the mid-latitudinal north atlantic during the onset of the late pliocene |
publishDate |
2024 |
url |
https://doi.org/10.5194/egusphere-2024-603 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-603/ |
genre |
Ice Sheet north atlantic current North Atlantic |
genre_facet |
Ice Sheet north atlantic current North Atlantic |
op_source |
eISSN: |
op_relation |
doi:10.5194/egusphere-2024-603 https://egusphere.copernicus.org/preprints/2024/egusphere-2024-603/ |
op_doi |
https://doi.org/10.5194/egusphere-2024-603 |
_version_ |
1810450105047711744 |