Using Pteropod Shells to Trace Aragonite Dissolution: Toward a Multi-Basin Calibration

We developed a new proxy for tracing aragonite dissolution in marine sediments. The core tops we used are from the tropical and subtropical latitudes of two ocean basins: Atlantic and Pacific. This allows for a multi-basin calibration for our proxy which is based on the fragmentation trend of pteropod shells. The ratio of fragmented pteropod shells to whole plus fragmented pteropod shells within our core tops has an excellent relationship with the aragonite saturation of bottom waters. Combining our pteropod-based aragonite dissolution proxy with the Globorotalia menradii Fragmentation Index, which is a calcite dissolution proxy, allows tracing carbonate chemistry of bottom waters for the entire ocean depth profile including regions well above the calcite saturation horizon. We also present new data on size normalized weights of pteropod shells which supports the aragonite dissolution trend seen in the pteropod fragmentation data. Unlike previous findings with other proxies, both aragonite and calcite dissolution data from a high resolution core in the western equatorial Pacific reveal no evidence of a degacial carbonate preservation maximum.