Ripple cross-laminated sediments on the East Antarctic Shelf: evidence for episodic bottom water production during the Holocene?
- 17 November 2000
- journal article
- Published by Elsevier in Marine Geology
- Vol. 170 (3-4) , 317-330
- https://doi.org/10.1016/s0025-3227(00)00096-7
Abstract
No abstract availableKeywords
This publication has 34 references indexed in Scilit:
- Variations in bioturbation across the oxygen minimum zone in the northwest Arabian SeaDeep Sea Research Part II: Topical Studies in Oceanography, 2000
- Provenance and dispersal of glacial–marine surface sediments in the Weddell Sea and adjoining areas, Antarctica: ice-rafting versus current transportMarine Geology, 1999
- How much deep water is formed in the Southern Ocean?Journal of Geophysical Research: Oceans, 1998
- Antarctic glacial history since the Last Glacial Maximum: an overview of the record on landAntarctic Science, 1998
- DID CHANGES IN ANTARCTIC ICE VOLUME INFLUENCE LATE HOLOCENE SEA-LEVEL LOWERING?Quaternary Science Reviews, 1998
- Distribution of diatoms in surface sediments of Prydz Bay, AntarcticaMarine Micropaleontology, 1997
- Geomorphology and sedimentology of the continental shelf adjacent to Mac. Robertson Land, East Antarctica: A scalped shelfGeo-Marine Letters, 1996
- Seasonal and interannual variations of the oceanic heat flux under a landfast Antarctic sea ice coverJournal of Geophysical Research: Oceans, 1996
- Pre‐bomb radiocarbon and the reservoir correction for calcareous marine species in the Southern OceanGeophysical Research Letters, 1996
- Biogenic facies in the Antarctic glacimarine environment: Basis for a polar glacimarine summaryPalaeogeography, Palaeoclimatology, Palaeoecology, 1988