THE ROLE OF LIGHT LIMITATION IN THE ONTOGENY OF EXTREMELY LONG-LIVED, TEMPERATE-WATER BIVALVES FROM THE EOCENE OF ANTARCTICA
Geochemical studies focused on two well-preserved specimens of the bivalve Cucullaea raea from the Eocene La Meseta Formation of Seymour Island, Antarctic Peninsula (64° S, 56° W). Each exhibits many distinct, closely spaced growth bands in cross section. Both d18O and d13C from microsampled shell carbonate yield strong seasonal variation over a significant period of the clams life, confirming that bands form annually. Counts of growth bands in these and additional specimens yield ages of 80 or more years. Plots of d18O versus distance along the shell show sharply peaked negative extremes reflecting growth cessation during the summer and broad positive extremes representing more continuous growth during the winter. Inferred paleotemperatures, assuming an ice-free world, reveal a mean annual temperature comparable to present SSTs off the New Jersey shore (~13-14°C), but less seasonal (~10°C range). Carbon isotope profiles are perfectly negatively correlated with oxygen, reflecting higher primary productivity during the summer months. The association of growth bands with negative d18O and positive d13C suggests that Cucullaea stopped growing during periods of warmest temperatures and highest food and light availability. Such a counterintuitive pattern hints at reproductive strategy, with the organism devoting metabolic energy to spawning rather than growth during optimal conditions such that offspring have the highest chance for survival. Cucullaeas age, slow growth, and temperate but light-limited environment suggest that extreme longevity in modern bivalves may be more influenced by light availability than previously thought.