Proxies in late cenozoic paleoceanography / (Record no. 15304)

MARC details
000 -LEADER
fixed length control field 01695 a2200253 4500
001 - CONTROL NUMBER
control field TB12767
003 - CONTROL NUMBER IDENTIFIER
control field IN-BhIIT
005 - DATE AND TIME OF LATEST TRANSACTION
control field 20260213000145.0
008 - FIXED-LENGTH DATA ELEMENTS--GENERAL INFORMATION
fixed length control field 260212b |||||||| |||| 00| 0 eng d
020 ## - INTERNATIONAL STANDARD BOOK NUMBER
ISBN ;9780444527554 (hbk.)
040 ## - CATALOGING SOURCE
Original cataloging agency IN-BhIIT
041 ## - LANGUAGE CODE
Language code of text eng
082 ## - DEWEY DECIMAL CLASSIFICATION NUMBER
Classification number 551.46
Book number HIL/P
100 ## - MAIN ENTRY--AUTHOR NAME
Personal name Marcel, C. Hillaire
Relator term Editor
245 ## - TITLE STATEMENT
Title Proxies in late cenozoic paleoceanography /
Statement of responsibility, etc C. Hillaire-Marcel, Anne de Vernal
260 ## - PUBLICATION, DISTRIBUTION, ETC. (IMPRINT)
Place of publication Amsterdam :
Name of publisher Elsevier,
Year of publication 2007.
300 ## - PHYSICAL DESCRIPTION
Number of Pages vol. I. xviii, 843 p. :
Other physical details(ill.) ill. ;
Dimensions(size) 30 cm.
490 ## - SERIES STATEMENT
Series statement Developments in Marine Geology
504 ## - BIBLIOGRAPHY, ETC. NOTE
Bibliography, etc Includes bibliographical references. and index.
520 ## - SUMMARY, ETC.
Summary, etc The 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 ## - SUBJECT ADDED ENTRY--TOPICAL TERM
Topical Term Paleoceanography
700 ## - ADDED ENTRY--PERSONAL NAME
Personal name Vernal, Anne de
Relator term Editor
942 ## - ADDED ENTRY ELEMENTS (KOHA)
Koha item type Text Book
Holdings
Withdrawn status Lost status Damaged status Not for loan Collection code Home library Current library Date acquired Source of acquisition Cost, normal purchase price Volume Info Full call number Accession Number Cost, replacement price Price effective from Koha item type
Not withdrawn Not Lost not damaged   SEOCS Central Library, IIT Bhubaneswar Central Library, IIT Bhubaneswar 04/02/2026 51 10389.43 vol.I 551.46 HIL/P TB12766 14232.10 04/02/2026 Course Reserve
Not withdrawn Not Lost not damaged   SEOCS Central Library, IIT Bhubaneswar Central Library, IIT Bhubaneswar 04/02/2026 51 10389.43 vol. I 551.46 HIL/P TB12767 14232.10 04/02/2026 Text Book

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