Radiocarbon datings of bottom sediments from the Sea of Japan

Fuente: PANGAEA
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Dettagli Bibliografici
Autori principali: Derkachev, A N, Utkin, I V, Gorbarenko, Sergey A, Pletnev, S P, Kovalyukh, N N, Botsul, A I, Bersenev, YuI
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1983
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author Derkachev, A N
Utkin, I V
Gorbarenko, Sergey A
Pletnev, S P
Kovalyukh, N N
Botsul, A I
Bersenev, YuI
author_facet Derkachev, A N
Utkin, I V
Gorbarenko, Sergey A
Pletnev, S P
Kovalyukh, N N
Botsul, A I
Bersenev, YuI
collection Datos científicos de ciencias marinas y ambientales
contents Based on comprehensive conjugate analysis of sediment cores by lithological, foraminiferal, diatom, oxygen isotope, and radiocarbon methods a correlation of Upper Quaternary Japan Sea sediments has been carried out. At the top of the studied section marker horizons have been distinguished: a boundary of carbonate and siliceous packets, an interlayer of volcanic ash. They have a wide areal distribution. Their age has been determined by the radiocarbon method. A map of sedimentation rates during late postglacial time is given.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_775517
institution PANGAEA
language en
publishDate 1983
publisher PANGAEA
record_format pangaea
spellingShingle Radiocarbon datings of bottom sediments from the Sea of Japan
Derkachev, A N
Utkin, I V
Gorbarenko, Sergey A
Pletnev, S P
Kovalyukh, N N
Botsul, A I
Bersenev, YuI
Age, 14C benzol synthesis; Age, dated; Age, dated, standard deviation; Archive of Ocean Data; ARCOD; Calculated; Dao-83-1615; Dao-83-1623; Dao-83-1639; Dao-83-1670; Dao-83-1681; Dao-83-1682; Dao-83-1801; Dao-83-1838; Dao-83-2117; Dao-83-2124; Dao-83-2127; Dao-83-2152; Dao-83-2153; Dao-83-7672; Dao-83-7675; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; Latitude of event; Longitude of event; Sample comment; Sea of Japan
Based on comprehensive conjugate analysis of sediment cores by lithological, foraminiferal, diatom, oxygen isotope, and radiocarbon methods a correlation of Upper Quaternary Japan Sea sediments has been carried out. At the top of the studied section marker horizons have been distinguished: a boundary of carbonate and siliceous packets, an interlayer of volcanic ash. They have a wide areal distribution. Their age has been determined by the radiocarbon method. A map of sedimentation rates during late postglacial time is given.
title Radiocarbon datings of bottom sediments from the Sea of Japan
topic Age, 14C benzol synthesis; Age, dated; Age, dated, standard deviation; Archive of Ocean Data; ARCOD; Calculated; Dao-83-1615; Dao-83-1623; Dao-83-1639; Dao-83-1670; Dao-83-1681; Dao-83-1682; Dao-83-1801; Dao-83-1838; Dao-83-2117; Dao-83-2124; Dao-83-2127; Dao-83-2152; Dao-83-2153; Dao-83-7672; Dao-83-7675; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Event label; Latitude of event; Longitude of event; Sample comment; Sea of Japan
url https://doi.org/10.1594/PANGAEA.775517