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Paleo-climate reconstruction on sediment core M72/5_628-1 (25-GC-1), Black Sea
The Marine Isotope Stage (MIS) 3 stands out due to its abrupt changes from cold and dry stadials to warm and humid interstadials, the so-called Dansgaard-Oeschger cycles that... -
Rock and paleomagnetic results of sediment core MSM33_856-1 over the past 30 ka
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Rock and paleomagnetic results of sediment core MSM33_855-1 over the past 30 ka
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Paleomagnetic results of sediment core MSM33_868-1 (63-1) from the Black Sea
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Paleomagnetic results of sediment core MSM33_869-1 (64-1) from the Black Sea
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Paleomagnetic results of sediment core MSM33_867-1 (62-1) from the Black Sea
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Paleomagnetic results of sediment core MSM33_865-1 (61-1) from the Black Sea
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Paleomagnetic results of sediment core MSM33_864-1 (60-1) from the Black Sea
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Paleomagnetic results of sediment core MSM33_860-1 (57-1) from the Black Sea
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Paleomagnetic results of sediment core MSM33_859-1 (56-1) from the Black Sea
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Paleomagnetic results of sediment core MSM33_856-1 (55-1) from the Black Sea
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Paleomagnetic results of sediment core MSM33_855-1 (54-3) from the Black Sea
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Paleomagnetic results of sediment core MSM33_849-1 (51-3) from the Black Sea
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Black Sea paleosecular variation stack between 68.9 and 14.5 ka
A full vector paleomagnetic record, comprising directional data and relative paleointensity (rPI), were derived from 16 sediment cores recovered from the southeastern Black Sea.... -
Paleomagnetic results of sediment core M72/5_640-1 (22-GC8) from the Black Sea
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Paleomagnetic results of sediment core M72/5_628-1 (25-GC1) from the Black Sea
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Paleomagnetic results of sediment core M72/5_625-1 (24-GC3) from the Black Sea
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Paleomagnetic results of sediment core M72/5_620-1 (22-GC4) from the Black Sea
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Paleomagnetic results of sediment core M72/5_619-1 (22-GC3) from the Black Sea
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Paleomagnetic results of sediment core M72/5_638-1 (22-GC6) from the Black Sea
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