Biogenic and detrital-rich intervals in central Arctic Ocean cores identified using x-ray fluorescence scanning

X-ray fluorescence (XRF) scanning of sediment cores from the Lomonosov Ridge and the Morris Jesup Rise reveals a distinct pattern of Ca intensity peaks through Marine Isotope Stages (MIS) 1 to 7. Downcore of MIS 7, the Ca signal is more irregular and near the detection limit. Virtually all major pea...

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Bibliographic Details
Published in:Polar Research
Main Authors: Daniela Hanslik, Ludvig Löwemark, Martin Jakobsson
Format: Article in Journal/Newspaper
Language:English
Published: Norwegian Polar Institute 2013
Subjects:
IRD
geo
Online Access:https://doi.org/10.3402/polar.v32i0.18386
https://doaj.org/article/5dcb4036b6224111944118bc73858ec8