Accumulation rates of bulk sediment and total organic carbon for Ontong Java Plateau sediments

Fuente: PANGAEA
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Auteurs principaux: Stax, Rainer, Stein, Ruediger
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 1993
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author Stax, Rainer
Stein, Ruediger
author_facet Stax, Rainer
Stein, Ruediger
collection Datos científicos de ciencias marinas y ambientales
contents Organic geochemical investigations were performed on sediments of Leg 130 to reconstruct the depositional environment of the Ontong Java Plateau. The Miocene to Quaternary sediments collected during the drilling campaign are characterized by extremely low organic carbon contents. As indicated by C/N ratios and Rock-Eval data, most of the organic matter is probably of marine origin. Based on mass-accumulation rates of organic carbon, the paleoproductivity for the Miocene-Pliocene and the late Pliocene-Pleistocene time intervals as well as the modern surface-water production were estimated. The productivity values of the surface sediments (25-59 gC/m2/yr) reflect the various influences of the equatorial upwelling cell on the different sites. The accumulation rates of organic carbon are generally low; however, they show a distinct increase at 8 Ma and a decrease at 2 Ma.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_780751
institution PANGAEA
language en
publishDate 1993
publisher PANGAEA
record_format pangaea
spellingShingle Accumulation rates of bulk sediment and total organic carbon for Ontong Java Plateau sediments
Stax, Rainer
Stein, Ruediger
130-803D; 130-804C; 130-805B; 130-805C; 130-806B; 130-807A; DRILL; Drilling/drill rig; Joides Resolution; Leg130; North Pacific Ocean; Ocean Drilling Program; ODP; West equatorial Pacific Ocean
Organic geochemical investigations were performed on sediments of Leg 130 to reconstruct the depositional environment of the Ontong Java Plateau. The Miocene to Quaternary sediments collected during the drilling campaign are characterized by extremely low organic carbon contents. As indicated by C/N ratios and Rock-Eval data, most of the organic matter is probably of marine origin. Based on mass-accumulation rates of organic carbon, the paleoproductivity for the Miocene-Pliocene and the late Pliocene-Pleistocene time intervals as well as the modern surface-water production were estimated. The productivity values of the surface sediments (25-59 gC/m2/yr) reflect the various influences of the equatorial upwelling cell on the different sites. The accumulation rates of organic carbon are generally low; however, they show a distinct increase at 8 Ma and a decrease at 2 Ma.
title Accumulation rates of bulk sediment and total organic carbon for Ontong Java Plateau sediments
topic 130-803D; 130-804C; 130-805B; 130-805C; 130-806B; 130-807A; DRILL; Drilling/drill rig; Joides Resolution; Leg130; North Pacific Ocean; Ocean Drilling Program; ODP; West equatorial Pacific Ocean
url https://doi.org/10.1594/PANGAEA.780751