Drift distances, times and primary grain sources of the Arctic Ocean, Exp302 (ACEX)

Fuente: PANGAEA
Guardado en:
Detalles Bibliográficos
Autor principal: Darby, Dennis A
Formato: Dataset Open Access
Lenguaje:en
Publicado: PANGAEA 2009
Materias:
Acceso en línea:
Etiquetas: Agregar Etiqueta
Sin Etiquetas, Sea el primero en etiquetar este registro!
_version_ 1867169498475266048
author Darby, Dennis A
author_facet Darby, Dennis A
collection Datos científicos de ciencias marinas y ambientales
contents Knowledge of the long-term history of the perennial ice is an important issue that has eluded study because the Cenozoic core material needed has been unavailable until the recent Arctic Coring Expedition (ACEX). Detrital Fe oxide mineral grains analyzed by microprobe from the last 14 Ma (164 m) of the ACEX composite core on the Lomonosov Ridge were matched to circum-Arctic sources with the same mineral and 12-element composition. These precise source determinations and estimates of drift rates were used to determine that these sand grains could not be rafted to the ACEX core site in less than a year. Thus the perennial ice cover has existed since 14 Ma except for the unlikely rapid return to seasonal ice between the average sampling interval of about 0.17 Ma. Both North America and Russia contributed significant Fe grains to the ACEX core during the last 14 Ma.
format Dataset Open Access
id pangaea_https___doi_org_10_1594_PANGAEA_711530
institution PANGAEA
language en
publishDate 2009
publisher PANGAEA
record_format pangaea
spellingShingle Drift distances, times and primary grain sources of the Arctic Ocean, Exp302 (ACEX)
Darby, Dennis A
302-CompSite; ACEX; Arctic Coring Expedition, ACEX; CCGS Captain Molly Kool (Vidar Viking); COMPCORE; Composite Core; Exp302; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP
Knowledge of the long-term history of the perennial ice is an important issue that has eluded study because the Cenozoic core material needed has been unavailable until the recent Arctic Coring Expedition (ACEX). Detrital Fe oxide mineral grains analyzed by microprobe from the last 14 Ma (164 m) of the ACEX composite core on the Lomonosov Ridge were matched to circum-Arctic sources with the same mineral and 12-element composition. These precise source determinations and estimates of drift rates were used to determine that these sand grains could not be rafted to the ACEX core site in less than a year. Thus the perennial ice cover has existed since 14 Ma except for the unlikely rapid return to seasonal ice between the average sampling interval of about 0.17 Ma. Both North America and Russia contributed significant Fe grains to the ACEX core during the last 14 Ma.
title Drift distances, times and primary grain sources of the Arctic Ocean, Exp302 (ACEX)
topic 302-CompSite; ACEX; Arctic Coring Expedition, ACEX; CCGS Captain Molly Kool (Vidar Viking); COMPCORE; Composite Core; Exp302; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP
url https://doi.org/10.1594/PANGAEA.711530