(Table 1) Age determination of ODP Hole 117-723A

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Autori principali: Naidu, Pothuri Divakar, Malmgren, Bjorn
Natura: Dataset Open Access
Lingua:en
Pubblicazione: PANGAEA 1995
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author Naidu, Pothuri Divakar
Malmgren, Bjorn
author_facet Naidu, Pothuri Divakar
Malmgren, Bjorn
collection Datos científicos de ciencias marinas y ambientales
contents We have carried out a high-resolution study of fluctuations in upwelling intensity along the Oman Margin, western Arabian Sea, through the last 19,130 years based on several marine microfossil indices of upwelling. We document a periodicity of 2,200 years in the upwelling indices, which would be governed by the south-west (SW) monsoon with such a periodicity. Our data further demonstrate greater amplitude in the variability of the SW monsoon during the Holocene than during the last glacial period. Our reported 2,200 years periodicity has two implications (1) oceanic circulation changes partly influence monsoon strength at sub-Milankovitch cycles (2) previously documented 2,300 years periodicity in atmospheric 14C might be induced by oceanic circulation changes.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_837323
institution PANGAEA
language en
publishDate 1995
publisher PANGAEA
record_format pangaea
spellingShingle (Table 1) Age determination of ODP Hole 117-723A
Naidu, Pothuri Divakar
Malmgren, Bjorn
117-723A; Age, 14C AMS; Age, dated; Age, dated, standard deviation; Arabian Sea; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg117; Ocean Drilling Program; ODP; Sample code/label
We have carried out a high-resolution study of fluctuations in upwelling intensity along the Oman Margin, western Arabian Sea, through the last 19,130 years based on several marine microfossil indices of upwelling. We document a periodicity of 2,200 years in the upwelling indices, which would be governed by the south-west (SW) monsoon with such a periodicity. Our data further demonstrate greater amplitude in the variability of the SW monsoon during the Holocene than during the last glacial period. Our reported 2,200 years periodicity has two implications (1) oceanic circulation changes partly influence monsoon strength at sub-Milankovitch cycles (2) previously documented 2,300 years periodicity in atmospheric 14C might be induced by oceanic circulation changes.
title (Table 1) Age determination of ODP Hole 117-723A
topic 117-723A; Age, 14C AMS; Age, dated; Age, dated, standard deviation; Arabian Sea; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg117; Ocean Drilling Program; ODP; Sample code/label
url https://doi.org/10.1594/PANGAEA.837323