Ute Frank, Norbert R. Detailed palaeo- and rock magnetic investigations were carried out on two sediment cores from the Tobago Basin, Eastern Caribbean. The 2. Global climatic variations marking the transition from the Pleistocene into the Holocene are clearly reflected in the rock magnetic parameters. Their variations reflect the contribution of the coarse-grained fraction to the bulk composition. However, fine-grained Ti-magnetite particles carry a fairly stable magnetization in sediments deposited in the last 10 kyr.
BayCEER Workshop 2009
Archaeomagnetic dating accuracy precision
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Phantom time hypothesis
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