Research On The Paleoclimatic Record In Frozen Pond Sediments And Ice Cores

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Here, we present five 12 m sediment cores from a sag pond along the San Andreas Fault in the southern Carrizo Plain. The most complete record (core CLPC21-4) was selected for a variety of chronological, sedimentological, and biological analyses.

Marine sediments were frozen syn-and epigenetically with cryotexture and ground ice formation. Ice wedges formation corresponds to the end of the Pleistocene (MIS2) and during cooler periods of the Holocene.

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Research On The Paleoclimatic Record In Frozen Pond Sediments And Ice Cores

compared with ice core records available from the polar regions and can therefore expand. our understanding of inter-hemispheric dynamics of past climate changes. The main objectives of our paleoclimate research in the Tien Shan mountains of middle.

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Research On The Paleoclimatic Record In Frozen Pond Sediments And Ice Cores

📁 Category: Cores

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