Variations in oxygen and carbon isotopic compositions and microstructure of the shell of Adamussium colbecki (Bivalvia)

The oxygen and carbon isotopic variability within the calcitic shell of the Antarctic scallop Adamussium colbecki has been assessed by detailed sampling of the shell margin, an external transect along the line of maximum growth, and on the interior surface of the shell. The adult shell is largely ca...

Full description

Saved in:
Bibliographic Details
Published in:Palaios 1990-04, Vol.5 (2), p.149-159
Main Authors: Barrera, Enriqueta, Tevesz, Michael J.S, Carter, Joseph G
Format: Article
Language:English
Subjects:
Adamussium colbecki
Antarctic Ocean
Aragonite
Bicarbonates
biochemistry
Bivalvia
C-13
Calcite
carbon
Geochemistry
Geology
Invertebrata
isotopes
McMurdo Sound
microstructure
Mollusca
O-18
Oxygen
paleoecology
paleontology
Research Reports
Ross Sea
Salinity
Sea water
shells
Southern Ocean
Spring water
stable isotopes
Summer
Surface water
variations
Citations: Items that cite this one
Online Access:Get full text
Tags: Add Tag
No Tags, Be the first to tag this record!
Description
Summary:The oxygen and carbon isotopic variability within the calcitic shell of the Antarctic scallop Adamussium colbecki has been assessed by detailed sampling of the shell margin, an external transect along the line of maximum growth, and on the interior surface of the shell. The adult shell is largely calcitic, with aragonite restricted to myostracal deposits, an extremely thin layer of aragonitic homogeneous structure between the pallial line and the foliated inner layer of the right valve, and the fibrous ligament. No relationship between isotopic values and microstructure is apparent. Average δ18O values are highest for the interior shell surface and lowest for the shell margin samples. The variability of δ18O values is highest for the external shell surface. The relatively good agreement between δ18O values of exterior surface samples along the growth transect of A. colbecki and estimated δ18O values of calcite precipitated in equilibrium with ambient waters calculated indicate the precipitation of shell samples close to equilibrium. Because δ18O values from A. colbecki reasonably well reflect ambient conditions, fossil forms would likely provide useful paleoenvironmental data. However, within shell variability in δ18O values cautions against making interpretations based on a few microsamples. Carbon isotopic values are highly variable throughout the shell and are likely influenced by vital effects.
ISSN:0883-1351
1938-5323
DOI:10.2307/3514811