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Quaternary Hypsithermals

  • Cesare Emiliani (a1)
Abstract

Oxygen isotopic analysis and absolute dating of deep-sea cores show that temperatures as high as those of today occurred for only about 10% of the time during the past half million years. The shortness of the high temperature intervals (“hypsithermals”) suggests a precarious environmental balance, a condition which makes man's interference with the environment during the present hypsithermal extremely critical. This precarious balance must be stabilized if a new glaciation or total deglaciation is to be avoided.

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This list contains references from the content that can be linked to their source. For a full set of references and notes please see the PDF or HTML where available.

W.S. Broecker K.K. Turekian B.C. Heezen 1958 The relation of deep-sea sedimentation rates to variations in climate American Journal of Science 256 503

E.S. Deevey R.F. Flint 1957 Postglacial Hypsithermal interval Science 125 182

C. Emiliani 1955 Pleistocene temperatures Journal of Geology 63 538

C. Emiliani 1958 Paleotemperature analysis of core 280 and Pleistocene correlations Journal of Geology 66 264

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Quaternary Research
  • ISSN: 0033-5894
  • EISSN: 1096-0287
  • URL: /core/journals/quaternary-research
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