_version_ 1867171055690317824
author Jacobel, Allison W
Costa, Kassandra M
Lynch-Stieglitz, Jean
Marchitto, Thomas M
author_facet Jacobel, Allison W
Costa, Kassandra M
Lynch-Stieglitz, Jean
Marchitto, Thomas M
collection Datos científicos de ciencias marinas y ambientales
contents Quantitative constraints on deep ocean carbonate chemistry are critical for understanding the processes responsible for glacial-interglacial changes in atmospheric pCO2 and the ocean feedbacks that amplify carbon cycle change. Here, we present a new, millennially-resolved, B/Ca-based record of carbonate ion concentration (∆[CO32-]), measured on C. wullerstorfi, from central equatorial Pacific site ML1208-16BB spanning the last 35 ka. This site, bathed by Pacific Deep Water, reveals a ~24 ± 7 µmol/kg rise in deep ocean [CO32-] between ~20 and 10 ka, a larger change than previously reconstructed from sites in the western equatorial Pacific and those in the central equatorial Pacific bathed by Lower Circumpolar Deep Water.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_986846
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Trace Elements of sediment core ML1208-16BB from central equatorial Pacific
Jacobel, Allison W
Costa, Kassandra M
Lynch-Stieglitz, Jean
Marchitto, Thomas M
Age, uncertainty; Age model; B/Ca; Calculated according to Yu and Elderfield (2007); carbonate preservation; Central equatorial Pacific; Cibicidoides wuellerstorfi, Aluminium/Calcium ratio; Cibicidoides wuellerstorfi, Boron/Calcium ratio; Cibicidoides wuellerstorfi, Boron/Calcium ratio, uncertainty; Cibicidoides wuellerstorfi, carbonate saturation state; Cibicidoides wuellerstorfi, carbonate saturation state, uncertainty; Cibicidoides wuellerstorfi, Iron/Calcium ratio; Cibicidoides wuellerstorfi, Manganese/Calcium ratio; DEPTH, sediment/rock; Depth, sediment/rock, bottom/maximum; Depth, sediment/rock, top/minimum; Equatorial pacific ocean; GC; Gravity corer; Inductively coupled plasma - mass spectrometry (ICP-MS), Thermo Finnigan, Element 2 followed by Marchitto (2006); LGM; Marcus G. Langseth; MGL2408; ML1208-16BB; see comment; trace metals
Quantitative constraints on deep ocean carbonate chemistry are critical for understanding the processes responsible for glacial-interglacial changes in atmospheric pCO2 and the ocean feedbacks that amplify carbon cycle change. Here, we present a new, millennially-resolved, B/Ca-based record of carbonate ion concentration (∆[CO32-]), measured on C. wullerstorfi, from central equatorial Pacific site ML1208-16BB spanning the last 35 ka. This site, bathed by Pacific Deep Water, reveals a ~24 ± 7 µmol/kg rise in deep ocean [CO32-] between ~20 and 10 ka, a larger change than previously reconstructed from sites in the western equatorial Pacific and those in the central equatorial Pacific bathed by Lower Circumpolar Deep Water.
title Trace Elements of sediment core ML1208-16BB from central equatorial Pacific
topic Age, uncertainty; Age model; B/Ca; Calculated according to Yu and Elderfield (2007); carbonate preservation; Central equatorial Pacific; Cibicidoides wuellerstorfi, Aluminium/Calcium ratio; Cibicidoides wuellerstorfi, Boron/Calcium ratio; Cibicidoides wuellerstorfi, Boron/Calcium ratio, uncertainty; Cibicidoides wuellerstorfi, carbonate saturation state; Cibicidoides wuellerstorfi, carbonate saturation state, uncertainty; Cibicidoides wuellerstorfi, Iron/Calcium ratio; Cibicidoides wuellerstorfi, Manganese/Calcium ratio; DEPTH, sediment/rock; Depth, sediment/rock, bottom/maximum; Depth, sediment/rock, top/minimum; Equatorial pacific ocean; GC; Gravity corer; Inductively coupled plasma - mass spectrometry (ICP-MS), Thermo Finnigan, Element 2 followed by Marchitto (2006); LGM; Marcus G. Langseth; MGL2408; ML1208-16BB; see comment; trace metals
url https://doi.org/10.1594/PANGAEA.986846