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Main Authors: Higgins, Sean M, Anderson, Robert F, Marcantonio, Franco, Schlosser, Peter, Stute, Martin
Format: Dataset Open Access
Language:en
Published: PANGAEA 2002
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Online Access:https://doi.org/10.1594/PANGAEA.710909
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author Higgins, Sean M
Anderson, Robert F
Marcantonio, Franco
Schlosser, Peter
Stute, Martin
author_facet Higgins, Sean M
Anderson, Robert F
Marcantonio, Franco
Schlosser, Peter
Stute, Martin
collection Datos científicos de ciencias marinas y ambientales
contents The accumulation of extraterrestrial 3He, a tracer for interplanetary dust particles (IDPs), in sediments from the Ontong Java Plateau (OJP; western equatorial Pacific Ocean) has been shown previously to exhibit a regular cyclicity during the late Pleistocene, with a period of ~100 ka. Those results have been interpreted to reflect periodic variability in the global accretion of IDPs that, in turn, has been linked to changes in the inclination of Earth's orbit with respect to the invariable plane of the solar system. Here we show that the accumulation in OJP sediments of authigenic 230Th, produced by radioactive decay of 234U in seawater, exhibits a 100-ka cyclicity similar in phase and amplitude to that evident in the 3He record. We interpret the similar patterns of 230Th and 3He accumulation to reflect a common origin within the ocean-climate system. Comparing spatial and temporal patterns of sediment accumulation against regional patterns of biological productivity and against the well-established pattern of CaCO3 dissolution in the deep Pacific Ocean leads to the further conclusion that a common 100-ka cycle in accumulation of biogenic, authigenic and extraterrestrial constituents in OJP sediments reflects the influence of climate-related changes in sediment focusing, rather than changes in the rate of production or supply of sedimentary constituents.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_710909
institution PANGAEA
language en
publishDate 2002
publisher PANGAEA
record_format pangaea
spellingShingle Radioisotopes and He accumulation in deep sea sediments of the Ontong Java Plateau
Higgins, Sean M
Anderson, Robert F
Marcantonio, Franco
Schlosser, Peter
Stute, Martin
130-806B; 130-806C; DRILL; Drilling/drill rig; Joides Resolution; Leg130; North Pacific Ocean; Ocean Drilling Program; ODP; PC; Piston corer; RC17; RC17-177; Robert Conrad
The accumulation of extraterrestrial 3He, a tracer for interplanetary dust particles (IDPs), in sediments from the Ontong Java Plateau (OJP; western equatorial Pacific Ocean) has been shown previously to exhibit a regular cyclicity during the late Pleistocene, with a period of ~100 ka. Those results have been interpreted to reflect periodic variability in the global accretion of IDPs that, in turn, has been linked to changes in the inclination of Earth's orbit with respect to the invariable plane of the solar system. Here we show that the accumulation in OJP sediments of authigenic 230Th, produced by radioactive decay of 234U in seawater, exhibits a 100-ka cyclicity similar in phase and amplitude to that evident in the 3He record. We interpret the similar patterns of 230Th and 3He accumulation to reflect a common origin within the ocean-climate system. Comparing spatial and temporal patterns of sediment accumulation against regional patterns of biological productivity and against the well-established pattern of CaCO3 dissolution in the deep Pacific Ocean leads to the further conclusion that a common 100-ka cycle in accumulation of biogenic, authigenic and extraterrestrial constituents in OJP sediments reflects the influence of climate-related changes in sediment focusing, rather than changes in the rate of production or supply of sedimentary constituents.
title Radioisotopes and He accumulation in deep sea sediments of the Ontong Java Plateau
topic 130-806B; 130-806C; DRILL; Drilling/drill rig; Joides Resolution; Leg130; North Pacific Ocean; Ocean Drilling Program; ODP; PC; Piston corer; RC17; RC17-177; Robert Conrad
url https://doi.org/10.1594/PANGAEA.710909