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Paleobathymetry, Paleotemperature, and Tectonism
Geological Society of America Bulletin, 1970Paleobathymetric trends of Cenozoic sedimentary sections from widely separated geographic areas show striking similarities. In areas examined, early and middle Eocene and middle Oligocene to middle Miocene ages are intervals of deeper water sedimentation and warm oceanic temperatures. Late Eocene to early Oligocene and the late Miocene to Holocene ages
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Erratum: Pleistocene Paleotemperatures
Science, 1993In the letter "Pleistocene paleotemperatures" by Cesare Emiliani (11 Sept., p. 1462), two reference numbers in the text were incorrect. In the second complete paragraph, in the second column, (1) should have been (2), and (6, 7) should have been (1, 7).
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Alkenone Paleotemperature Determinations
2003The alkenone paleotemperature (‘U k 37 ’) method, which relies on determining the unsaturation index of biomarker compounds produced by one group of closely related haptophyte algae, is now widely used to reconstruct near-surface ocean temperatures on timescales ranging from a few centuries to millions of years.
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Isotopic Paleotemperatures: Discussion
Science, 1967W L, Donn, D M, Shaw, C, Emiliani
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Quaternary Paleotemperatures and the Duration of the High-Temperature Intervals
Science, 1972Oxygen isotopic analysis of Caribbean cores P6304-4 and P6304-7, and the close correlation of these cores with other Caribbean and Atlantic cores previously analyzed, make possible the reconstruction of a paleotemperature curve of considerable detail. This curve demonstrates again the unusualness of the present interval of high temperature within the ...
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Paleotemperature Variations across the Plio-Pleistocene Boundary
Science, 1971Strong variations in the O 18 /O 16 and C 13 /C 12 ratios occur through the type section for the Plio-Pleistocene boundary, but the boundary itself is not characterized by unusual isotopic gradients.
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How to Assess Maturation and Paleotemperatures
1987Abstract The application of organic matter studies in petroleum exploration had its start with the recognition of “rank” in coal. During the period of 1900–1925, both physical and chemical methods were developed for determination of the degree of low grade metamorphism of particulate organic materials, or palynodebris in coals and ...
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