See more from this Division: Topical Sessions
See more from this Session: Sclerochronological Archives from Rivers to the Sea: Documentation, Interpretation, and Utility
Abstract:
The concept is straightforward: the 1st derivative of a function relating cumulative linear growth to time represents intra-annual growth ratesthe growth function. In practice, this technique involves converting observed oxygen-isotope values from shell carbonate (δ18Ocarb) to temperatures, which requires knowledge of the oxygen-isotopic composition of water. Then calculated temperatures are converted to dates using observed temperature records. Next, dates are plotted versus sample distance (measured from sampled shells), and fit with a monotonic cubic spline. Finally, the 1st derivative of this function is evaluated. This procedure is then repeated (~50000x), by taking advantage of the uncertainly associated with δ18Ocarb measurement (e.g., ±0.08). This iterative procedure produces an average growth function, which can, in turn, provide valuable ecological information, such as the timing of highest intra-annual growth rates, growth-limiting temperatures, and optimal-growth temperatures.
Because these data are often established using growth increments, which are equivocal in many freshwater mollusks, this modeling procedure may provide researchers and resource managers an important new tool for assessing and/or predicting accretional histories. Furthermore, because this method is based on readily available environmental records and requires relatively few specimens, it is ideal for studying threatened or endangered species.
See more from this Division: Topical Sessions
See more from this Session: Sclerochronological Archives from Rivers to the Sea: Documentation, Interpretation, and Utility