Data_Sheet_1_Long-Term Trends in Estuarine Carbonate Chemistry in the Northwestern Gulf of Mexico.pdf

• Main Authors: Melissa R. McCutcheon, Xinping Hu
• Format: Dataset
• Language: unknown
• Published: 2022
• Subjects: Oceanography; Marine Biology; Marine Geoscience; Biological Oceanography; Chemical Oceanography; Physical Oceanography; Marine Engineering; long-term trend; carbonate chemistry; pCO2; buffer capacity; estuary; Ocean acidification
• Online Access: https://doi.org/10.3389/fmars.2022.793065.s001; https://figshare.com/articles/dataset/Data_Sheet_1_Long-Term_Trends_in_Estuarine_Carbonate_Chemistry_in_the_Northwestern_Gulf_of_Mexico_pdf/19296689

A four-decade dataset that spans seven estuaries along a latitudinal gradient in the northwestern Gulf of Mexico and includes measurements of pH and total alkalinity was used to calculate partial pressure of CO 2 (pCO 2 ), dissolved inorganic carbon (DIC), saturation state of aragonite (Ω Ar ), and a buffer factor (β DIC , which measures the response of proton concentration or pH to DIC concentration change) and examine long-term trends and spatial patterns in these parameters. With the notable exception of the northernmost and southernmost estuaries (and selected stations near freshwater input), these estuaries have generally experienced long-term increases in pCO 2 and decreases in DIC, Ω Ar , and β DIC , with the magnitude of change generally increasing from north to south. At all stations with increasing pCO 2 , the rate of increase exceeded the rate of increase in atmospheric pCO 2 , indicating that these estuaries have become a greater source of CO 2 to the atmosphere over the last few decades. The decreases in Ω Ar have yet to cause Ω Ar to near undersaturation, but even the observed decreases may have the potential to decrease calcification rates in important estuarine calcifiers like oysters. The decreases in β DIC directly indicate that these estuaries have experienced continually greater change in pH in the context of ocean acidification.