High-field magnetic susceptibility (χHF) as a proxy of biogenic sedimentation along the Antarctic Peninsula
- 1 July 2006
- journal article
- Published by Elsevier in Physics of the Earth and Planetary Interiors
- Vol. 156 (3-4) , 274-282
Abstract
No abstract availableKeywords
This publication has 12 references indexed in Scilit:
- A 13 200 year history of century to millennial-scale paleoenvironmental change magnetically recorded in the Palmer Deep, western Antarctic PeninsulaEarth and Planetary Science Letters, 2002
- Unmixing magnetic assemblages and the magnetic behavior of bimodal mixturesJournal of Geophysical Research, 2001
- Data Report: Biogenic Opal in Palmer Deep Sediments, Site 1098, Leg 1782001
- Palmer Deep Composite Depth Scales for Leg 178 Sites 1098 and 10992001
- Chronology of the Palmer Deep site, Antarctic Peninsula: a Holocene palaeoenvironmental reference for the circum-AntarcticThe Holocene, 2001
- Rock-magnetic carriers of century-scale susceptibility cycles in glacial–marine sediments from the Palmer Deep, Antarctic PeninsulaEarth and Planetary Science Letters, 2000
- Seismic stratigraphy of Palmer Deep: a fault-bounded late Quaternary sediment trap on the inner continental shelf, Antarctic Peninsula Pacific marginMarine Geology, 1998
- Productivity cycles of 200–300 years in the Antarctic Peninsula region: Understanding linkages among the sun, atmosphere, oceans, sea ice, and biotaGeological Society of America Bulletin, 1996
- A simple method for the rapid determination of biogenic opal in pelagic marine sedimentsDeep Sea Research Part A. Oceanographic Research Papers, 1989
- The supply and accumulation of silica in the marine environmentGeochimica et Cosmochimica Acta, 1981