Paleogene and Early Neogene Deep Water Paleoceanography of the Indian Ocean as Determined from Benthic Foraminifer Stable Carbon and Oxygen Isotope Records

2013 ◽  
pp. 351-385 ◽  
Author(s):  
James C. Zachos ◽  
David K. Rea ◽  
Koji Seto ◽  
Ritsuo Nomura ◽  
Nobuaki Niitsuma
Keyword(s):  
Indian Ocean ◽  
Oxygen Isotope ◽  
Deep Water ◽  
Benthic Foraminifer ◽  
Stable Carbon ◽  
Carbon And Oxygen Isotope ◽  
Early Neogene ◽  
The Indian Ocean

Stable carbon and oxygen isotope compositions of extant crinoidal echinoderm skeletons

2012 ◽  
Vol 291 ◽  
pp. 132-140 ◽  
Author(s):  
Przemysław Gorzelak ◽  
Jarosław Stolarski ◽  
Krzysztof Małkowski ◽  
Anders Meibom
Keyword(s):  
Oxygen Isotope ◽  
Stable Carbon ◽  
Carbon And Oxygen Isotope

scholarly journals Sampling and Pretreatment of Tooth Enamel Carbonate for Stable Carbon and Oxygen Isotope Analysis

10.3791/58002 ◽  
2018 ◽  
Author(s):  
Alicia Ventresca Miller ◽  
Ricardo Fernandes ◽  
Anneke Janzen ◽  
Ayushi Nayak ◽  
Jillian Swift ◽  
...  
Keyword(s):  
Oxygen Isotope ◽  
Tooth Enamel ◽  
Isotope Analysis ◽  
Stable Carbon ◽  
Carbon And Oxygen Isotope

Detrital and authigenic minerals in sediments from the western part of the Indian Ocean

1986 ◽  
Vol 50 (355) ◽  
pp. 69-74 ◽  
Author(s):  
A. E. Tsirambides
Keyword(s):  
Indian Ocean ◽  
Oxygen Isotope ◽  
Western Indian Ocean ◽  
The Other ◽  
Authigenic Minerals ◽  
Volcanic Material ◽  
Two Samples ◽  
The Indian Ocean ◽  
Isotope Analyses ◽  
Mn Oxides

AbstractMineralogical and oxygen isotope analyses have been performed on nine western Indian Ocean core samples in order to distinguish the detrital from authigenic minerals in the sediments. Following the removal of carbonates, organic constituents and Fe and Mn oxides, the residue was separated into five size fractions, the principal minerals present being feldspar, quartz, clinoptilolite, and clay minerals.Oxygen isotope compositions for two samples reflect an authigenic origin for clinoptilolite by the submarine alteration of volcanic material. Oxygen isotope compositions of two separates (free from feldspar and clays) suggest a detrital origin for the quartz in this area. The same mode of origin is apparent for the other components too, except possibly for some smectite which may have formed authigenically.

Microscale stable carbon and oxygen isotope measurement of individual otoliths of larvae and juveniles of Japanese anchovy and sardine

2020 ◽  
Vol 245 ◽  
pp. 106946 ◽  
Author(s):  
Kozue Nishida ◽  
Ayaka Yasu ◽  
Nobuaki Nanjo ◽  
Motomitsu Takahashi ◽  
Satoshi Kitajima ◽  
...  
Keyword(s):  
Oxygen Isotope ◽  
Japanese Anchovy ◽  
Stable Carbon ◽  
Larvae And Juveniles ◽  
Carbon And Oxygen Isotope ◽  
Isotope Measurement
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