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Increases in atmospheric carbon dioxide (pCO2) are projected to contribute to a 1.1-6.4°C rise in global average surface temperatures and a 0.14-0.35 reduction in the average pH of the global surface ocean by 2100. If realized, these changes are expected to have negative consequences for reef-building corals including increased frequency and severity of coral bleaching and reduced rates of calcification and reef accretion. Much less is known regarding the independent and combined effects of temperature and pCO2 on critical early life history processes such as fertilization. Here we show that increases in temperature (+3°C) and pCO2 (+400 µatm) projected for this century negatively impact fertilization success of a common Indo-Pacific coral species, Acropora tenuis. While maximum fertilization did not differ among treatments, the sperm concentration required to obtain 50% of maximum fertilization increased 6- to 8- fold with the addition of a single factor (temperature or CO2) and nearly 50- fold when both factors interact. Our results indicate that near-future changes in temperature and pCO2 narrow the range of sperm concentrations that are capable of yielding high fertilization success in A. tenuis. Increased sperm limitation, in conjunction with adult population decline, may have severe consequences for coral reproductive success. Impaired sexual reproduction will further challenge corals by inhibiting population recovery and adaptation potential.
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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC3572969 | PMC |
http://journals.plos.org/plosone/article?id=10.1371/journal.pone.0056468 | PLOS |
Crit Care Explor
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Division of Pulmonary and Critical Care Medicine, Mayo Clinic, Rochester, MN.
Objective: To identify distinct phenotypes of acute respiratory distress syndrome (ARDS) developing after hematopoietic cell transplantation (HCT), using routinely available clinical data at ICU admission.
Design: Multicenter retrospective cohort study using latent class analysis.
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Anal Chim Acta
October 2025
College of Marine Science, University of South Florida, St. Petersburg, USA. Electronic address:
Background: Total alkalinity (A) is a fundamental parameter in understanding the oceanic cycling of carbon dioxide (CO). Measurements of the A of natural waters are typically obtained through single- or multi-step titrations using a strong acid, with the endpoint pH determined via potentiometry or spectrophotometry. Conventional A determinations are labor-intensive and require precise knowledge of the sample's weight or volume.
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September 2025
Institute of Energy, Peking University, Beijing 100871, China.
Reconstructing carbon release fluxes during ancient climatic warming events is important for improving predictions of carbon cycle and climate dynamics under future anthropogenic warming scenarios. We investigate the extent of biogenic methane release and its contribution to climate variability across the Toarcian Oceanic Anoxic Event (T-OAE) approximately 183 million years ago. To do this, we developed a global biogeochemical model and applied a Bayesian inversion using Markov Chain Monte Carlo (MCMC) simulations.
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October 2025
Universidad Nacional Autónoma de México, Unidad Académica Mazatlán, Instituto de Ciencias del Mar y Limnología, Calz. Joel Montes Camarena s/n, 82040, Mazatlán, Mexico.
The partial pressure of CO (p(CO)) dissolved in seawater is often indirectly determined through a mathematical calculation involving two variables of the carbonate system, which requires the use of expensive equipment, materials, and reagents, and is usually demanding in terms of human resources. In this study, we present a simple, low-cost method for directly measuring dissolved CO (p(CO)) in coastal waters using a small gas equilibrator coupled with a non-dispersive infrared (NDIR) detector in a closed-loop system. The cost of this methodology can be further reduced by utilizing a low-cost NDIR detector and inexpensive materials.
View Article and Find Full Text PDFSci Rep
August 2025
Department of Geological Sciences, Stockholm University, Stockholm, Sweden.
We investigated the relative contributions of various factors that influence seasonal changes in sea surface partial pressure of ( , calculated from the measured pH and total alkalinity) in four regions of northwestern Greenland: Nares Strait, Lincoln Sea, Sherard Osborn and Petermann fjords. Using the temperature minimum layer as a proxy for winter conditions, we examined dynamics from the onset of sea-ice melt to summer. Our findings revealed significant spatial variability in , driven by differences in temperature, freshwater inputs, and biological activity.
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