Westfield, I. | bioRxiv Science

bioRxiv2020

General DNA methylation patterns and environmentally-induced differential methylation in the eastern oyster (Crassostrea virginica)

Epigenetic modification, specifically DNA methylation, is one possible mechanism for intergenerational plasticity. Before inheritance of methylation patterns can be characterized, we need a better understanding of how environmental change modifies the parental epigenome. To examine the influence of experimental ocean acidification on eastern oyster (Crassostrea virginica) gonad tissue, oysters were cultured in the laboratory under control (491 {+/-} 49 atm) or high (2550 {+/-} 211 atm) pCO2 conditions for four weeks. DNA from reproductive tissue was isolated from five oysters per treatment, then subjected to bisulfite treatment and DNA sequencing. Irrespective of treatment, DNA methylation was primarily found in gene bodies with approximately 22% of CpGs (2.7% of total cytosines) in the C. virginica genome predicted to be methylated. In response to elevated pCO2, we found 598 differentially methylated loci primarily overlapping with gene bodies. A majority of differentially methylated loci were in exons (61.5%) with less intron overlap (31.9%). While there was no evidence of a significant tendency for the genes with differentially methylated loci to be associated with distinct biological processes, the concentration of these loci in gene bodies, including genes involved in protein ubiquitination and biomineralization suggests DNA methylation may be important for transcriptional control in response to ocean acidification. Changes in gonad methylation also indicate potential for these methylation patterns to be inherited by offspring. Understanding how experimental ocean acidification conditions modify the oyster epigenome, and if these modifications are inherited, allows for a better understanding of how ecosystems will respond to environmental change.

genomics↗

bioRxiv2018

Nearshore corals on the Mesoamerican Barrier Reef System on pace to cease growing as soon as year 2110

Anthropogenic global change and local anthropogenic stressors are decreasing coral growth and survival globally, thus altering the structure and function of coral reef ecosystems. We show that skeletal extension rates of nearshore colonies of Siderastrea siderea and Pseudodiploria strigosa across the Belize Mesoamerican Barrier Reef System (MBRS) have declined at average rates of 0.01 and 0.08 mm/yr, respectively, over approximately the past century, while offshore conspecifics exhibited no significant trend in extension with time. This caused extension rates of nearshore colonies to converge with their historically slower-growing offshore conspecifics. Bleaching events negatively impacted extension rates in S. siderea but not in P. strigosa. The more negative trend in linear extension for nearshore versus offshore colonies may arise from ocean warming combined with stronger land-based anthropogenic stressors within nearshore environments. Extrapolating these trends in linear extension into the future suggests that nearshore P. strigosa and S. siderea will cease growing by years 2110 and 2370, respectively.

ecology↗