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Changes in the extent of marine anoxia during the Early Jurassic: Evidence from molybdenum isotopes

✍ Scribed by C.R. Pearce; A.S. Cohen; A.L. Coe; K.W. Burton


Book ID
116502207
Publisher
Elsevier Science
Year
2006
Tongue
English
Weight
40 KB
Volume
70
Category
Article
ISSN
0016-7037

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The interval of time represented by marine isotope stages 11 and 12 (V360^470 ka) contains what may be the most extreme glacial and interglacial climate conditions of the Late Pleistocene. It has been suggested that sea level rose by V160 m at the termination of glacial stage 12. This is 30% greater