(Table 1) Age determination of sediment profile SO90-41KL/63KA

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Autori principali: Staubwasser, Michael, Sirocko, Frank, Grootes, Pieter Meiert, Erlenkeuser, Helmut
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 2002
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author Staubwasser, Michael
Sirocko, Frank
Grootes, Pieter Meiert
Erlenkeuser, Helmut
author_facet Staubwasser, Michael
Sirocko, Frank
Grootes, Pieter Meiert
Erlenkeuser, Helmut
collection Datos científicos de ciencias marinas y ambientales
contents The 14C ages of planktonic foraminifers Globigerinoides sacculifer bracketing the Younger Dryas in a d18O record of Globigerinoides ruber from a laminated sediment core on the Pakistani continental margin suggest that surface reservoir ages in the Arabian Sea were in excess of 1000 years during the deglaciation. A least squares error fit of a detailed 14C chronology to the (atmospheric) tree ring record gave variable early Holocene reservoir ages between 780 and 1120 years, well above the prebomb value of 640 years. Mid-Holocene reservoir ages are less well constrained but were probably closer to the prebomb value. The method used to fit individual core sections to the tree ring record was designed to require only a rough a priori estimate of the time spans, which in the core presented here were taken from each section's range of 14C ages. A significant 220-year quasi-oscillation was present in the d18O record during the early Holocene but not thereafter. This frequency and amplitude pattern resembles an early Holocene 207- to 227-year oscillation previously observed in the atmospheric 14C record, which is generally interpreted as reflecting solar irradiance variability. An early Holocene climate event at 8150-8400 calendar years B.P. observed elsewhere within the Asian-East African monsoon system was again found in our record, suggesting a reduction in precipitation over NW India and Pakistan.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_842448
institution PANGAEA
language en
publishDate 2002
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Age determination of sediment profile SO90-41KL/63KA
Staubwasser, Michael
Sirocko, Frank
Grootes, Pieter Meiert
Erlenkeuser, Helmut
Age, 14C AMS; Age, 14C calibrated; Age, comment; Age, dated; Age, dated, standard deviation; Age, dated material; Arabian Sea; Calendar age; COMPCORE; Composite Core; DEPTH, sediment/rock; PAKOMIN; Reservoir age; Reservoir age, standard error; Section; SO90; SO90-41KL/63KA; Sonne
The 14C ages of planktonic foraminifers Globigerinoides sacculifer bracketing the Younger Dryas in a d18O record of Globigerinoides ruber from a laminated sediment core on the Pakistani continental margin suggest that surface reservoir ages in the Arabian Sea were in excess of 1000 years during the deglaciation. A least squares error fit of a detailed 14C chronology to the (atmospheric) tree ring record gave variable early Holocene reservoir ages between 780 and 1120 years, well above the prebomb value of 640 years. Mid-Holocene reservoir ages are less well constrained but were probably closer to the prebomb value. The method used to fit individual core sections to the tree ring record was designed to require only a rough a priori estimate of the time spans, which in the core presented here were taken from each section's range of 14C ages. A significant 220-year quasi-oscillation was present in the d18O record during the early Holocene but not thereafter. This frequency and amplitude pattern resembles an early Holocene 207- to 227-year oscillation previously observed in the atmospheric 14C record, which is generally interpreted as reflecting solar irradiance variability. An early Holocene climate event at 8150-8400 calendar years B.P. observed elsewhere within the Asian-East African monsoon system was again found in our record, suggesting a reduction in precipitation over NW India and Pakistan.
title (Table 1) Age determination of sediment profile SO90-41KL/63KA
topic Age, 14C AMS; Age, 14C calibrated; Age, comment; Age, dated; Age, dated, standard deviation; Age, dated material; Arabian Sea; Calendar age; COMPCORE; Composite Core; DEPTH, sediment/rock; PAKOMIN; Reservoir age; Reservoir age, standard error; Section; SO90; SO90-41KL/63KA; Sonne
url https://doi.org/10.1594/PANGAEA.842448