Letter sectionBiogenic carbonate sediments on the Scottish continental shelf and on Rockall Bank
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Cited by (39)
Experimental determination of the dissolution rates of calcite, aragonite, and bivalves
2005, Chemical GeologyCitation Excerpt :There are several motivations for this work. First, bivalves are abundant in coastal systems (Wilson, 1979, 1988), where their dissolution significantly affects chemical evolution during diagenesis (Walls et al., 1977; South and Talbot, 2000; Brachert and Dullo, 2000). Secondly, the trace element compositions of shells are commonly used to deduce the past composition of their depositional waters (Rahimpour-Bonab et al., 1997; Anadón et al., 2002); an improved understanding of their dissolution behaviour provides insight into their suitability as paleoindicators.
Sand-drift and soil formation along an exposed north Atlantic coastline: 14,000 years of diverse geomorphological, climatic and human impacts
1999, Journal of Archaeological ScienceBioclastic carbonate sediments on the southwestern Svalbard shelf
1996, Marine GeologyNon-tropical carbonate deposits on the modern New Zealand shelf
1988, Sedimentary Geology
Copyright © 1979 Published by Elsevier B.V.