Dataset Information

Dynamic response in the larval geoduck clam proteome to elevated pCO2

ABSTRACT: Pacific geoduck (Panopea generosa) clams are found along the Northeast Pacific coast where they are significant components of coastal and estuarine ecosystems and the basis of a highly profitable aquaculture industry. The Pacific coastline, however, is also the sight of rapidly changing ocean habitat, including significant reductions in pH. To better understand the physiological impact of ocean acidification on geoduck clams, we characterized for the first time the proteomic profile of this bivalve during early larval development and compared it to that of larvae exposed to low pH.Geoduck larvae wer reared at pH 7.5 (ambient) or 7.1 in a commercial shellfish hatchery from day 6 to 19 post-fertilization , and sampled at six time points for an in-depth proteomics analysis using high-resolution data dependent analysis. We found that larvae reared at low pH were smaller than those reared at ambient pH, especially in the prodissoconch II phase of development, and displayed a delay in their competency for settlement. Proteomic profiles revealed that metabolic, cell cycle, and protein turnover pathways differed between the two pH, suggesting that differing phenotypic outcomes between pH 7.5 and 7.1 are likely due to environmental disruptions to the timing of molecular physiological events. In summary, ocean acidification likely caused an energetic stress on geoduck larvae, casuing a shift in physiological prioritization.

INSTRUMENT(S): Orbitrap Fusion Lumos

ORGANISM(S): Panopea Generosa

TISSUE(S): Whole Body

SUBMITTER: Emma Timmins-Schiffman

LAB HEAD: Steven Roberts

PROVIDER: PXD013667 | Pride | 2019-05-04

REPOSITORIES: Pride

ACCESS DATA

Similar Datasets

Project description:Increasing atmospheric CO2 concentrations are causing decreased pH over vast expanses of the ocean. This decreasing pH may alter biogeochemical cycling of carbon and nitrogen via the microbial process of nitrification, a key process that couples these cycles in the ocean, but which is often sensitive to acidic conditions. Recent reports indicate a decrease in oceanic nitrification rates under experimentally lowered pH. How composition and abundance of ammonia oxidizing bacteria (AOB) and archaea (AOA) assemblages respond to decreasing oceanic pH, however, is unknown. We sampled microbes from two different acidification experiments and used a combination of qPCR and functional gene microarrays for the ammonia monooxygenase gene (amoA) to assess how acidification alters the structure of ammonia oxidizer assemblages. We show that despite widely different experimental conditions, acidification consistently altered the community composition of AOB by increasing the relative abundance of taxa related to the Nitrosomonas ureae clade. In one experiment this increase was sufficient to cause an increase in the overall abundance of AOB. There were no systematic shifts in the community structure or abundance of AOA in either experiment. These different responses to acidification underscore the important role of microbial community structure in the resiliency of marine ecosystems. amoA gene diversity from two ocean acidification experiments, Monterey Bay experiment (two time points, ambient and acidified) and Vineyard Sound experiment (ambient and acifidied, with and without nutrients) examined with 2 two-color arrays (Cy3 and Cy5): the universal standard 20-mer oligo is printed to the slide with a 70-mer oligo (an archetype). Environmental DNA sequences (fluoresced with Cy3) within 15% of the 70-mer conjugated to a 20-mer oligo (fluoresced with Cy5) complementary to the universal standard will bind to the oligo probes on the array. Signal is the ratio of Cy3 to Cy5.

Project description:In this research we present a transcriptomics analysis of the physiological response of a marine calcifier, Strongylocentrotus purpuratus, to ocean acidification, a decline in ocean pH that results from the absorption of anthropogenic carbon dioxide (CO2). Larvae were raised from fertilization to prism stage in seawater with elevated CO2 conditions based upon IPCC emissions scenario B1 (540ppm CO2) and A1FI (1020ppm CO2). Adult S. purpuratus were collected using SCUBA from Goleta Pier (Goleta,CA, USA) and maintained in flowing seawater tables at 15-16°C. Spawning was induced by coelomic injection of 0.5M KCl following standard methods (Strathmann 1987). Eggs were collected from 3 females and separately fertilized by sperm from a single male (i.e. all larvae were full or half-siblings). Each of the three replicate cultures were divided in three (nine cultures total) and held in 10L flow-through containers filled with seawater aerated through a side arm with commercially manufactured air containing three different pCO2: 380ppm CO2 (present day atmospheric CO2 level, pH 8.01 ± 0.01), 540ppm CO2, an optimistic atmospheric CO2 concentration predicted by the Intergovernmental Panel on Climate Change for 2100 (B1 scenario, pH 7.96 ± 0.01) and 1020ppm CO2 (A1FI scenario, pH 7.88 ± 0.01). Larvae were cultured at 15°C until prism stage (40h post-fertilization). At the 40 hour time point, a sample of 60,000 larvae was removed from each of the 9 cultures in the 380, 540 and 1020 ppm treatments and stored in 1 mL Trizol at -80 ºC for later RNA analysis. The larval cDNA sample from each replicate 540ppm CO2 culture was competitively hybridized against the 380ppm CO2 control culture from the same replicate female. Similarly, the larval cDNA sample from each replicate 1020ppm CO2 culture was competitively hybridized against the 380ppm CO2 control culture from the same replicate female. Using dye swaps of technical replicates, treatment effects could be estimated independently of dye effects.

Dataset Information

Dynamic response in the larval geoduck clam proteome to elevated pCO2

Similar Datasets

OmicsDI is part of the ELIXIR infrastructure