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...
| Main Authors: | , , |
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| Format: | Article |
| Language: | English |
| Published: |
Norwegian Polar Institute
2013-02-01
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| Series: | Polar Research |
| Subjects: | |
| Online Access: | http://www.polarresearch.net/index.php/polar/article/view/18386/pdf_1 |