Foraminifera density analyses of sediment core ML1208-16BB from central equatorial Pacific

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Hauptverfasser: Jacobel, Allison W, Costa, Kassandra M, Lynch-Stieglitz, Jean, Marchitto, Thomas M
Format: Dataset Open Access
Sprache:en
Veröffentlicht: PANGAEA 2026
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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 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 the results of foraminifera density analyses (mass per feret diameter) as measured on the planktonic foraminifera G. ruber. These data are inconsistent with a co-registered B/Ca-based record of carbonate ion concentration (∆[CO32-]) suggesting a decoupling of bottom water and porewater carbonate chemistry.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_986847
institution PANGAEA
language en
publishDate 2026
publisher PANGAEA
record_format pangaea
spellingShingle Foraminifera density analyses of sediment core ML1208-16BB from central equatorial Pacific
Jacobel, Allison W
Costa, Kassandra M
Lynch-Stieglitz, Jean
Marchitto, Thomas M
Age model; B/Ca; carbonate preservation; Central equatorial Pacific; DEPTH, sediment/rock; Depth, sediment/rock, bottom/maximum; Depth, sediment/rock, top/minimum; Equatorial pacific ocean; GC; Globigerinoides ruber, Feret, diameter uncertainty; Globigerinoides ruber, Feret diameter; Globigerinoides ruber, mass per Feret diameter; Globigerinoides ruber, mass per Feret diameter, uncertainty; Gravity corer; LGM; Marcus G. Langseth; Mass; Mass, uncertainty; MGL2408; ML1208-16BB; see comment; trace metals; Ultramicrobalance, Mettler Toledo, XP2U
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 the results of foraminifera density analyses (mass per feret diameter) as measured on the planktonic foraminifera G. ruber. These data are inconsistent with a co-registered B/Ca-based record of carbonate ion concentration (∆[CO32-]) suggesting a decoupling of bottom water and porewater carbonate chemistry.
title Foraminifera density analyses of sediment core ML1208-16BB from central equatorial Pacific
topic Age model; B/Ca; carbonate preservation; Central equatorial Pacific; DEPTH, sediment/rock; Depth, sediment/rock, bottom/maximum; Depth, sediment/rock, top/minimum; Equatorial pacific ocean; GC; Globigerinoides ruber, Feret, diameter uncertainty; Globigerinoides ruber, Feret diameter; Globigerinoides ruber, mass per Feret diameter; Globigerinoides ruber, mass per Feret diameter, uncertainty; Gravity corer; LGM; Marcus G. Langseth; Mass; Mass, uncertainty; MGL2408; ML1208-16BB; see comment; trace metals; Ultramicrobalance, Mettler Toledo, XP2U
url https://doi.org/10.1594/PANGAEA.986847