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- W2059920883 abstract "Benthic foraminiferal and stable isotope studies of two borings from the island of Anholt, Denmark, reveal a continuous Late Saalian-Eemian sequence with an overall gradual warming interrupted by a short term temperature deterioration comparable with the Younger Dryas cold spell. The sequence is correlated to the global deep sea stable isotope record based on environmental evidence given by foraminiferal faunas and stable isotopes. The following environmental changes in the Anholt cores can be attributed to the global variations: (1) An interstadial phase, the “Flakket Interstadial”, which had a duration of about 1000 years, is correlated to stable isotope event 6.01. (2) The following cold spell, the “Kattegat Stadial”, spanning about 1000 years, represents most of the interval between isotope events 6.01 and 6.0. (3) A phase of rapid warming within about 1000 years bsotope events 6.0 and 5.53. (4) A sea level change within the Eemian between isotope events 5.53 and 5.51." @default.
- W2059920883 created "2016-06-24" @default.
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- W2059920883 date "1993-05-01" @default.
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- W2059920883 title "Benthic foraminiferal and stable isotope evidence for a “Younger Dryas-style” cold spell at the Saalian-Eemian transition, Denmark" @default.
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- W2059920883 doi "https://doi.org/10.1016/0031-0182(93)90008-7" @default.
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