| Summary: | <p>Carbonate chemistry of 3 pacific oyster cohorts from Whiskey Creek Hatchery. TCO2 and PCO2 are measured at analytical temp, values presented are corrected to in situ temp of 25 degrees C.</p> <p>All details on sample collection, methods, and analytical techniques may be found in:<br /> Waldbusser, G.G., E. L. Brunner,B.A. Haley, B. Hales, C. J. Langdon, and F. G. Prahl. 2013. A developmental and energetic basis linking larval oyster shell formation to ocean acidification. Geophysical Research Letters 40: 2171-2176. doi:<a href=\"http://dx.doi.org/10.1002/grl.50449\" target=\"_blank\">10.1002/grl.50449</a><br /> Brunner, E.L., F.G. Prahl, B. Hales, G.G. Waldbusser (in review). Insights from Stable Isotopes into the Sensitivity of Larval Pacific Oysters to Ocean Acidification. Marine Ecology Progress Series.</p> <p>The original file wass split into 3 spreadsheets containing three different, but related datasets<br /> <a href=\"http://www.bco-dmo.org/dataset/639820\" target=\"_blank\">Isotope Data Summary</a><br /> <a href=\"http://www.bco-dmo.org/dataset/639794\" target=\"_blank\">Biochem Summary</a><br /> Carbonate Chemistry Summary</p> <p>Across all three datasets, there are 3 cohorts of pacific oyster larvae that have been sampled, one in May and two in August, one in untreated seawater, the other in buffered seawater. Time is all indexed to fertilization of the oysters, with samples collected on days noted. </p>
|
|---|