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author Ronge, Thomas A
Nürnberg, Dirk
Tiedemann, Ralf
author_facet Ronge, Thomas A
Nürnberg, Dirk
Tiedemann, Ralf
collection Datos científicos de ciencias marinas y ambientales
contents Here we use Mg/Ca temperature estimates from subsurface and thermocline dwelling foraminifera to reconstruct the meridional Plio‐Pleistocene evolution of the Southeast Pacific thermocline, in relation to atmospheric circulation changes. Our data indicate a change in the thermocline, responding to the northward displacement of the Intertropical Convergence Zone/South Pacific High system between ~3.8 and 3.5 Ma. After 3.5 Ma, we record a second major phase of thermocline shoaling, which points to the ITCZ/SPH‐system movement toward its modern position along with the gradual cooling of the Northern Hemisphere and its associated glaciation.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_896166
institution PANGAEA
language en
publishDate 2018
publisher PANGAEA
record_format pangaea
spellingShingle Mg/Ca-derived temperature estimates for ODP Site 202-1236
Ronge, Thomas A
Nürnberg, Dirk
Tiedemann, Ralf
202-1236A; 202-1236B; 202-1236C; AGE; AWI_Paleo; Calculated, according to Anand et al. (2003); Calculated from Mg/Ca ratios (Groeneveld and Chiessi, 2011); Depth, composite; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Globorotalia inflata, Magnesium/Calcium ratio; Globorotalia tumida, Magnesium/Calcium ratio; Joides Resolution; Leg202; Mixed layer temperature; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Photic Zone temperature; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Sample code/label; Sea surface temperature, annual mean; South Pacific Ocean; SPP1158; Trilobatus sacculifer, Manganese/Calcium ratio
Here we use Mg/Ca temperature estimates from subsurface and thermocline dwelling foraminifera to reconstruct the meridional Plio‐Pleistocene evolution of the Southeast Pacific thermocline, in relation to atmospheric circulation changes. Our data indicate a change in the thermocline, responding to the northward displacement of the Intertropical Convergence Zone/South Pacific High system between ~3.8 and 3.5 Ma. After 3.5 Ma, we record a second major phase of thermocline shoaling, which points to the ITCZ/SPH‐system movement toward its modern position along with the gradual cooling of the Northern Hemisphere and its associated glaciation.
title Mg/Ca-derived temperature estimates for ODP Site 202-1236
topic 202-1236A; 202-1236B; 202-1236C; AGE; AWI_Paleo; Calculated, according to Anand et al. (2003); Calculated from Mg/Ca ratios (Groeneveld and Chiessi, 2011); Depth, composite; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Globorotalia inflata, Magnesium/Calcium ratio; Globorotalia tumida, Magnesium/Calcium ratio; Joides Resolution; Leg202; Mixed layer temperature; Paleoenvironmental Reconstructions from Marine Sediments @ AWI; Photic Zone temperature; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; Sample code/label; Sea surface temperature, annual mean; South Pacific Ocean; SPP1158; Trilobatus sacculifer, Manganese/Calcium ratio
url https://doi.org/10.1594/PANGAEA.896166