Diagenesis of Inoceramus and late Cretaceous paleoenvironmental geochemistry:  a case study from James Ross Island, Antarctica

D. Pirrie; Jim D. Marshall

doi:10.2307/3514889

Diagenesis of Inoceramus and late Cretaceous paleoenvironmental geochemistry: a case study from James Ross Island, Antarctica

D. Pirrie, Jim D. Marshall

Allbwn ymchwil: Cyfraniad at gyfnodolyn › Erthygl › adolygiad gan gymheiriaid

32 Dyfyniadau (Scopus)

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Paleotemperatures calculated from the isotopic composition of the belemnites give an average of 13.6°C for the "normal'marine waters. However, paleotemperatures based on the inoceramid bivalve data imply considerably higher values. Thus, although geochemistry is a powerful tool in paleoenvironmental analysis, habitat-related controls may significantly alter the observed geochemical signature. -from Authors

Iaith wreiddiol	Saesneg
Tudalennau (o-i)	336-345
Nifer y tudalennau	10
Cyfnodolyn	Palaios
Cyfrol	5
Rhif cyhoeddi	4
Dynodwyr Gwrthrych Digidol (DOIs)	https://doi.org/10.2307/3514889
Statws	Cyhoeddwyd - 1990

Mynediad at Ddogfen

10.2307/3514889Trwydded: CC BY-NC-ND

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@article{f7b649161cda43daa6d09ad54dedfada,

title = "Diagenesis of Inoceramus and late Cretaceous paleoenvironmental geochemistry: a case study from James Ross Island, Antarctica",

abstract = "Paleotemperatures calculated from the isotopic composition of the belemnites give an average of 13.6°C for the {"}normal'marine waters. However, paleotemperatures based on the inoceramid bivalve data imply considerably higher values. Thus, although geochemistry is a powerful tool in paleoenvironmental analysis, habitat-related controls may significantly alter the observed geochemical signature. -from Authors",

author = "D. Pirrie and Marshall, {Jim D.}",

year = "1990",

doi = "10.2307/3514889",

language = "English",

volume = "5",

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journal = "Palaios",

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TY - JOUR

T1 - Diagenesis of Inoceramus and late Cretaceous paleoenvironmental geochemistry

T2 - a case study from James Ross Island, Antarctica

AU - Pirrie, D.

AU - Marshall, Jim D.

PY - 1990

Y1 - 1990

N2 - Paleotemperatures calculated from the isotopic composition of the belemnites give an average of 13.6°C for the "normal'marine waters. However, paleotemperatures based on the inoceramid bivalve data imply considerably higher values. Thus, although geochemistry is a powerful tool in paleoenvironmental analysis, habitat-related controls may significantly alter the observed geochemical signature. -from Authors

AB - Paleotemperatures calculated from the isotopic composition of the belemnites give an average of 13.6°C for the "normal'marine waters. However, paleotemperatures based on the inoceramid bivalve data imply considerably higher values. Thus, although geochemistry is a powerful tool in paleoenvironmental analysis, habitat-related controls may significantly alter the observed geochemical signature. -from Authors

U2 - 10.2307/3514889

DO - 10.2307/3514889

M3 - Article

AN - SCOPUS:0025584453

SN - 0883-1351

VL - 5

SP - 336

EP - 345

JO - Palaios

JF - Palaios

IS - 4

ER -

Diagenesis of Inoceramus and late Cretaceous paleoenvironmental geochemistry: a case study from James Ross Island, Antarctica

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