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On Using Carbon and Oxygen Isotope Data from Glendonites as Paleoenvironmental Proxies: A Case Study from the Permian System of Eastern Australia

¹ Department of Geosciences, University of Nebraska–Lincoln, Lincoln, Nebraska 68588-0340, U.S.A.; tfrank2{at}unl.edu
² Department of Geological Sciences, Southern Methodist University, Dallas, Texas 75275, U.S.A.
³ Department of Geosciences, University of Nebraska–Lincoln, Lincoln, Nebraska 68588-0340, U.S.A.

Glendonites, calcite pseudomorphs after ikaite (CaCO₃ • 6H₂O), feature prominently in fine-grained, glacially influenced Permian marine strata of eastern Australia, which accumulated in a series of extensional basins that occupied polar to temperate latitudes along the southeastern margin of Gondwana. Because ikaite formation in the marine environment requires near-freezing temperatures, high alkalinity, and elevated concentrations of orthophosphate, the presence of glendonites in ancient strata implies a particular array of paleoenvironmental conditions. A petrographic and geochemical study was carried out to assess the veracity of isotopic data from glendonites as proxy indicators of ancient ocean chemistry, sea-floor temperature, and diagenesis. In thin section, glendonites consist of inclusion-zoned, equant to bladed calcite crystals, interpreted as the ikaite replacement phase, enclosed in a matrix of calcite and minor chalcedony and pyrite cements. Carbon and oxygen isotope data show a negative covariance, with ¹⁸O values ranging from –22.5 to +0.3 and ¹³C values from –27.7 to –4.5 V-PDB. Of the calcite phases examined, the ikaite replacement phase is the most enriched in ¹⁸O and most depleted in ¹³C; enclosing cements possess lower ¹⁸O and higher ¹³C values and are interpreted to have formed during later stages of burial diagenesis. The ¹⁸O values of the ikaite replacement phase do not correspond to formation with Permian seawater at near-freezing temperatures unless isotopic disequilibrium is assumed. The ¹³C values are similar to the carbon isotope composition of bulk organic matter in the host sediment, and suggest that the alkalinity and orthophosphate necessary for ikaite stability were generated in the zone of suboxic to anoxic diagenesis. Results indicate that although ¹⁸O and ¹³C values from glendonites are useful for understanding early to late diagenetic processes, they are not ideal proxies for seawater chemistry and temperature.

This article has been cited by other articles:

				N. P. James, T. D. Frank, and C. R. Fielding Carbonate Sedimentation in a Permian High-Latitude, Subpolar Depositional Realm: Queensland, Australia Journal of Sedimentary Research, March 1, 2009; 79(3): 125 - 143. [Abstract] [Full Text] [PDF]