Document Type
Thesis
Abstract
Resting metabolic rate (RMR) is a potentially useful physiological predictor of species' responses to climate warming because it represents the exchange of energy between an organism and its environment. Ectothermic species, like mollusks, will exchange heat energy at faster rates with the environment during warming, and enter a state of decreased respiration, heart rate, and metabolic rate. This allows mollusks with lower RMRs to better conserve energy and survive through periods of higher environmental pressure, including warming. By estimating RMR of fossil mollusks of the Yorktown Formation in Virginia, we can test whether the interaction between temperature and physiology influences fluctuations in molluscan abundance across the Mid-Pliocene Warm Period (MPWP). We hypothesized that bivalves and gastropods with higher RMRs would decrease in abundance across the MPWP. We examined 15 bulk samples from Yorktown Formation localities in southeastern Virginia collected from field sites and the Virginia Museum of Natural History collections. The Yorktown Formation is an ideal study system because: (1) the mollusks are well-preserved and sampled, highly abundant, and taxonomically well- resolved, and (2) paleotemperatures across the MPWP have been reconstructed recently for local outcrops. Each member of the Yorktown Formation represents a period of the MPWP: Sunken Meadow (before), Rushmere (during), and Moore House (after). All bulk samples were sieved, then specimens were sorted, identified using taxonomic monographs, and counted to the species level when possible. For each species present in the Sunken Meadow Member, we estimated RMR using maximum length measurements of species type specimens and pre-warming temperature data derived from recently unpublished paleoclimate reconstruction at the local scale. Genus- and species-level changes in the warming interval show no correlation between RMR and change in percent abundance, but high RMR taxa are more variable in their response to warming. This suggests that high RMR is a high risk/high reward trait, and other factors such as a species' body size, environmental setting, bathymetric range, and geographic range also affect changes in abundance. Understanding species-level responses to MPWP warming (1.8-3.6 Celsius above pre-industrial) may be useful for predicting the response of extant mollusks, particularly those with economically important fisheries, to similar climate warming in the mid-Atlantic U.S. today.
Date Awarded
Spring 2023
Department
Geology
Advisor 1
Rowan Lockwood
Recommended Citation
Spage, Natalie M., "Metabolic rate as a predictor of molluscan abundance across the Mid- Pliocene Warm Period in the Virginia Coastal Plain" (2023). Geology Senior Theses. William & Mary. Paper 54.
https://scholarworks.wm.edu/geologyseniors/54
