| 000 | 01695 a2200253 4500 | ||
|---|---|---|---|
| 001 | TB12767 | ||
| 003 | IN-BhIIT | ||
| 005 | 20260213000145.0 | ||
| 008 | 260212b |||||||| |||| 00| 0 eng d | ||
| 020 | _a;9780444527554 (hbk.) | ||
| 040 | _aIN-BhIIT | ||
| 041 | _aeng | ||
| 082 |
_a551.46 _bHIL/P |
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| 100 |
_aMarcel, C. Hillaire _eEditor _927243 |
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| 245 |
_aProxies in late cenozoic paleoceanography / _cC. Hillaire-Marcel, Anne de Vernal |
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| 260 |
_aAmsterdam : _bElsevier, _c2007. |
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| 300 |
_avol. I. xviii, 843 p. : _bill. ; _c30 cm. |
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| 490 | _a Developments in Marine Geology | ||
| 504 | _aIncludes bibliographical references. and index. | ||
| 520 | _aThe present volume is the first in a series of two books dedicated to the paleoceanography of the Late Cenozoic ocean. The need for an updated synthesis on paleoceanographic science is urgent, owing to the huge and very diversified progress made in this domain during the last decade. In addition, no comprehensive monography still exists in this domain. This is quite incomprehensible in view of the contribution of paleoceanographic research to our present understanding of the dynamics of the climate-ocean system. The focus on the Late Cenozoic ocean responds to two constraints. Firstly, most quantitative methods, notably those based on micropaleontological approaches, cannot be used back in time beyond a few million years at most. Secondly, the last few million years, with their strong climate oscillations, show specific high frequency changes of the ocean with a relatively reduced influcence of tectonics. | ||
| 650 |
_aPaleoceanography _94738 |
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| 700 |
_aVernal, Anne de _eEditor _927244 |
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| 942 | _cTB | ||
| 999 |
_c15304 _d15304 |
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