60 2YC and 4YCU Geoscience Student Research Poster Showcase

This session is designed for two-year college (2YC) and four-year college and university (4YCU) students presenting research posters in any sub-discipline of geoscience.

Sunday, 19 October 2025
8:00 AM - 5:30 PM
HBGCC, Hall 1


Shortened Longevity of the Bivalve Arctica islandica During the mid-Pliocene Warm Period

Paper number: 60-25
Program: Technical Sessions
Time: 8:00 AM – 8:00 AM


Authors


Abstract

Arctic islandica, a bivalve, is the longest lived non colonial animal on the planet today. In Iceland it has a maximum reported lifespan of 507 years and individuals with lifespans more than 200 years are common. In addition to being long-lived, modern A. islandica from Iceland are also slow growing and display some of the lowest von Bertalanffy k values of any bivalve. This extreme longevity and slow growth are perhaps a result of the combination of both cold temperatures and seasonal food availability driven by polar light regimes. Though A. islandica has a stratigraphic record that dates back to at least the Oligocene, the life history strategies of this species in deep time remain unknown. Here, we examined lifespans and growth rates of A. islandica from the Tjörnes beds in northern Iceland during the mid-Pliocene warm period. To examine internal growth increments, specimens were first embedded in an epoxy resin and then cut with a rock saw, polished with a lapidary wheel, and finally imaged using a light microscope. Our results suggest that Arctica islandica was much shorter lived during the Pliocene, with maximum lifespans of only 80 years, but that von Bertalanffy k values (k=0.02) were similar to today’s populations. It is possible that this reduced longevity is a result of higher temperature, and that the similarly low growth rates are a response to persistence of a seasonally available food regime at high latitudes.


Geological Society of America Abstracts with Programs. Vol. 57, No. 6

doi: 10.1130/abs/2025AM-413040

© Copyright 2025 The Geological Society of America (GSA), all rights reserved. Permission is hereby granted to the author(s) of this abstract to reproduce and distribute it freely, for noncommercial purposes. Permission is hereby granted to any individual scientist to download a single copy of this electronic file and reproduce up to 20 paper copies for noncommercial purposes advancing science and education, including classroom use, providing all reproductions include the complete content shown here, including the author information. All other forms of reproduction and/or transmittal are prohibited without written permission from GSA Copyright Permissions.