Low seawater pH can be harmful to many calcifying marine organisms, but the calcifying macroalgae Padina spp. flourish at natural submarine carbon dioxide seeps where seawater pH is low. We show that the microenvironment created by the rolled thallus margin of Padina australis facilitates supersaturation of CaCO3 and calcifi-cation via photosynthesis-induced elevated pH. Using microsensors to investigate oxygen and pH dynamics in the microenvironment of P. australis at a shallow CO2 seep, we found that, under saturating light, the pH inside the microenvironment (pHME ) was higher than the external seawater (pHSW ) at all pHSW levels investigated, and the difference (i.e., pHME - pHSW ) increased with decreasing pHSW (0.9 units at pHSW 7.0). Gross photosynthesis (Pg ) inside the microenvironment increased with decreasing pHSW , but algae from the control site reached a threshold at pH 6.5. Seep algae showed no pH threshold with respect to Pg within the pHSW range investigated. The external carbonic anhydrase (CA) inhibitor, acetazolamide, strongly inhibited Pg of P. australis at pHSW 8.2, but the effect was diminished under low pHSW (6.4-7.5), suggesting a greater dependence on membrane-bound CA for the dehydration of HCO3 (-) ions during dissolved inorganic carbon uptake at the higher pHSW . In comparison, a calcifying green alga, Halimeda cuneata f. digitata, was not inhibited by AZ, suggesting efficient bicarbonate transport. The ability of P. australis to elevate pHME at the site of calcification and its strong dependence on CA may explain why it can thrive at low pHSW .
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PLoS One
June 2024
School of Ocean and Earth Science, University of Southampton, National Oceanography Centre, Southampton, United Kingdom.
Geochemical proxies of sea surface temperature (SST) and seawater pH (pHsw) in scleractinian coral skeletons are valuable tools for reconstructing tropical climate variability. However, most coral skeletal SST and pHsw proxies are univariate methods that are limited in their capacity to circumvent non-climate-related variability. Here we present a novel multivariate method for reconstructing SST and pHsw from the geochemistry of coral skeletons.
View Article and Find Full Text PDFSci Total Environ
February 2024
Centre Scientifique de Monaco, 8 Quai Antoine Ier, 98000 Monaco, Principality of Monaco, Monaco; LIA ROPSE, Laboratoire International Associé Université Côte d'Azur - Centre Scientifique de Monaco, Monaco.
Ongoing ocean acidification is known to be a major threat to tropical coral reefs. To date, only few studies have evaluated the impacts of natural long-term exposure to low-pH seawater on the chemical regulation and growth of reef-building corals. This work investigated the different responses of the massive Porites coral living at normal (pH ~ 8.
View Article and Find Full Text PDFACS Omega
July 2021
College of Marine Science, University of South Florida, 800 1st Street South, St. Petersburg, Florida 33701, United States.
This work provides an algorithm to describe the salinity ( ) and temperature () dependence of the equilibrium and molar absorptivity characteristics of purified bromocresol purple (BCP, a pH indicator) over a river-to-sea range of salinity (0 ≤ ≤ 40). Based on the data obtained in this study, the pH of water samples can be calculated on the seawater pH scale as follows: pH = -log( ) + log(( - )/(1 - )) where -log( ) = 4.981 - 0.
View Article and Find Full Text PDFSoc Work Public Health
June 2020
Women's Health Program Coordinator at Fenway Health , Boston, Massachusetts, USA.
Progress in refining the definition and basic concepts of public health social work (PHSW) is central to its revitalization. Advancing PHSW further depends on understanding the roles, domains, and daily activities of current PHSW practitioners in the contemporary workforce. The goal of the is to explore how public health social workers conceptualize and locate their work.
View Article and Find Full Text PDFSci Adv
January 2020
Université de Brest, UBO, CNRS, IRD, Ifremer, Institut Universitaire Européen de la Mer, LEMAR, Rue Dumont d'Urville, 29280 Plouzané, France.
The response of marine-calcifying organisms to ocean acidification (OA) is highly variable, although the mechanisms behind this variability are not well understood. Here, we use the boron isotopic composition (δB) of biogenic calcium carbonate to investigate the extent to which organisms' ability to regulate pH at their site of calcification (pH) determines their calcification responses to OA. We report comparative δB analyses of 10 species with divergent calcification responses (positive, parabolic, threshold, and negative) to OA.
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