Navigation überspringen
Universitätsbibliothek Heidelberg
Status: Bibliographieeintrag

Verfügbarkeit
Standort: ---
Exemplare: ---
heiBIB
 Online-Ressource
Verfasst von:Xu, Qiang [VerfasserIn]   i
 Xiao, Wenshen [VerfasserIn]   i
 Wang, Rujian [VerfasserIn]   i
 Süfke, Finn [VerfasserIn]   i
 Lippold, Jörg [VerfasserIn]   i
 Not, Christelle [VerfasserIn]   i
Titel:Driving mechanisms of sedimentary 230Th and 231Pa variability in the Western Arctic Ocean through the last glacial cycle
Verf.angabe:Qian Xu, Wenshen Xiao, Rujian Wang, Finn Süfke, Jörg Lippold, and Christelle Not
E-Jahr:2021
Jahr:10 June 2021
Umfang:18 S.
Teil:volume:36
 year:2021
 number:7
 elocationid:e2020PA004039
 pages:1-18
 extent:18
Fussnoten:Gesehen am 29.09.2021
Titel Quelle:Enthalten in: Paleoceanography and paleoclimatology
Ort Quelle:Hoboken, NJ : Wiley, 2018
Jahr Quelle:2021
Band/Heft Quelle:36(2021), 7, Artikel-ID e2020PA004039, Seite 1-18
ISSN Quelle:2572-4525
Abstract:Concentration profiles of excess 230Th and 231Pa (230Thxs and 231Paxs) in Arctic Ocean sediment cores exhibit strong temporal variabilities, but the mechanisms responsible for the variabilities remain poorly understood. Here, we present new 230Thxs and 231Paxs profiles from the Mendeleev Ridge to examine downcore 230Thxs and 231Paxs distributions and their connection to environmental conditions in the Arctic. Measurable concentrations of 230Thxs(231Paxs) from the new record display an alternation of “230Thxs(231Paxs)-rich” and “230Thxs(231Paxs)-poor” sections as observed in the other cores from the Mendeleev Ridge. Sedimentary characteristics reveal that this alternation does not directly correspond to interglacial-glacial cycles. The 230Thxs and 231Paxs concentrations show an inverse relationship to their corresponding sedimentation rates, suggesting the distributions of 230Thxs and 231Paxs are affected by variable dilution with terrigenous material. However, changes in lateral transport of these isotopes may also account for the observed oscillations. Sedimentary cumulative inventories of 230Thxs show evidence for a net deficit of 230Th in the sediments during the last glacial period, possibly due to a lack of scavenging material in general.
DOI:doi:10.1029/2020PA004039
URL:Bitte beachten Sie: Dies ist ein Bibliographieeintrag. Ein Volltextzugriff für Mitglieder der Universität besteht hier nur, falls für die entsprechende Zeitschrift/den entsprechenden Sammelband ein Abonnement besteht oder es sich um einen OpenAccess-Titel handelt.

Volltext ; Verlag: https://doi.org/10.1029/2020PA004039
 Volltext: https://onlinelibrary.wiley.com/doi/abs/10.1029/2020PA004039
 DOI: https://doi.org/10.1029/2020PA004039
Datenträger:Online-Ressource
Sprache:eng
K10plus-PPN:1772076724
Verknüpfungen:→ Zeitschrift

Permanenter Link auf diesen Titel (bookmarkfähig):  https://katalog.ub.uni-heidelberg.de/titel/68784660   QR-Code
zum Seitenanfang