Age determination and median grain size of sediment core EN31-PC2

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Auteurs principaux: Brown, Paul, Kennett, James P, Ingram, B Lynn
Format: Dataset Open Access
Langue:en
Publié: PANGAEA 1999
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author Brown, Paul
Kennett, James P
Ingram, B Lynn
author_facet Brown, Paul
Kennett, James P
Ingram, B Lynn
collection Datos científicos de ciencias marinas y ambientales
contents Hemipelagic muds deposited during the past 5.3 cal kyr in the northern Gulf of Mexico (Orca Basin) contain seven intervals punctuated by relatively coarse siliciclastic grain-size peaks, planktonic faunal turnovers, and negative d13C excursions. We believe these episodes represent megaflood deposits reflecting historically unprecedented outfall of North American floodwater and terrigenous mud plumes into the gulf, resulting in collapse of the open-ocean pelagic ecosystem. The deposits record multidecadal episodes of high continental precipitation and large Mississippi River floods at ~4.7, 3.5, 3.0, 2.5, 2.0, 1.2, and 0.3 cal ka (500-1200-year recurrence interval). Variations in tropical plankton frequencies define submillenial warming intervals that culminate in these fluvial episodes. Strengthened tropical currents in the gulf at these times appear to have increased sea surface temperatures and associated flow of moist gulf air to the midwest. Terrestrial paleohydrologic records support the marine evidence for millennial-scale changes in recurrence of large midwest flood episodes.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_856719
institution PANGAEA
language en
publishDate 1999
publisher PANGAEA
record_format pangaea
spellingShingle Age determination and median grain size of sediment core EN31-PC2
Brown, Paul
Kennett, James P
Ingram, B Lynn
EN31-PC2; Endeavor; ENXX; Orca Basin; PC; Piston corer
Hemipelagic muds deposited during the past 5.3 cal kyr in the northern Gulf of Mexico (Orca Basin) contain seven intervals punctuated by relatively coarse siliciclastic grain-size peaks, planktonic faunal turnovers, and negative d13C excursions. We believe these episodes represent megaflood deposits reflecting historically unprecedented outfall of North American floodwater and terrigenous mud plumes into the gulf, resulting in collapse of the open-ocean pelagic ecosystem. The deposits record multidecadal episodes of high continental precipitation and large Mississippi River floods at ~4.7, 3.5, 3.0, 2.5, 2.0, 1.2, and 0.3 cal ka (500-1200-year recurrence interval). Variations in tropical plankton frequencies define submillenial warming intervals that culminate in these fluvial episodes. Strengthened tropical currents in the gulf at these times appear to have increased sea surface temperatures and associated flow of moist gulf air to the midwest. Terrestrial paleohydrologic records support the marine evidence for millennial-scale changes in recurrence of large midwest flood episodes.
title Age determination and median grain size of sediment core EN31-PC2
topic EN31-PC2; Endeavor; ENXX; Orca Basin; PC; Piston corer
url https://doi.org/10.1594/PANGAEA.856719