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Background: Dehydration caused by prolonged exercise impairs thermoregulation, endurance and exercise performance. Evidence from animal and human studies validates the potential of desalinated deep-ocean mineral water to positively impact physiological and pathophysiological conditions. Here, we hypothesize that deep-ocean mineral water drawn from a depth of 915 m off the Kona, HI coast enhances recovery of hydration and exercise performance following a dehydrating exercise protocol compared to mountain spring water and a carbohydrate-based sports drink.
Findings: Subjects (n = 8) were exposed to an exercise-dehydration protocol (stationary biking) under warm conditions (30 °C) to achieve a body mass loss of 3 % (93.4 ± 21.7 total exercise time). During the post-exercise recovery period, subjects received deep-ocean mineral water (Kona), mountain spring water (Spring) or a carbohydrate-based sports drink (Sports) at a volume (in L) equivalent to body mass loss (in Kg). Salivary samples were collected at regular intervals during exercise and post-exercise rehydration. Additionally, each participant performed peak torque knee extension as a measure of lower body muscle performance. Subjects who received Kona during the rehydrating period showed a significantly more rapid return to pre-exercise (baseline) hydration state, measured as the rate of decline in peak to baseline salivary osmolality, compared to Sports and Spring groups. In addition, subjects demonstrated significantly improved recovery of lower body muscle performance following rehydration with Kona versus Sports or Spring groups.
Conclusions: Deep-ocean mineral water shows promise as an optimal rehydrating source over spring water and/or sports drink.
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http://www.ncbi.nlm.nih.gov/pmc/articles/PMC4833963 | PMC |
http://dx.doi.org/10.1186/s12970-016-0129-8 | DOI Listing |
Geobiology
September 2025
Dipartimento di Scienze, Università di Roma Tre, Roma, Italy.
Large-scale geological processes shape microbial habitats and drive the evolution of life on Earth. During the Oligocene, convergence between Africa and Europe led to the opening of the Western Mediterranean Basin, a deep-ocean system characterized by fluid venting, oxygen depletion, and the absence of benthic fauna. In this extreme, inhospitable seafloor environment, fusiform objects known as Tubotomaculum formed, whose origin has long remained controversial.
View Article and Find Full Text PDFWater Res
August 2025
Key Laboratory of Marine Mineral Resources, Ministry of Natural Resources, Guangzhou Marine Geological Survey, China Geological Survey, Guangzhou, 511458, China; National Engineering Research Center for Gas Hydrate Exploration and Development, Guangzhou 511458, China. Electronic address: dengyinan@1
Microplastics (MPs) have penetrated even the most remote deep-sea sediments, yet their vertical distribution and depositional pathways remain unclear. This study analyzed sediment cores (0-20 cm) from 11 Philippine Sea stations, finding MPs in all layers with an average abundance of 218.4 ± 303.
View Article and Find Full Text PDFProc Natl Acad Sci U S A
September 2025
Department of Earth and Space Sciences, University of Washington, Seattle, WA 98195-1310.
The oxygenation history of Earth's surface environments has had a profound influence on the ecology and evolution of metazoan life. It was traditionally thought that the Neoproterozoic Oxygenation Event enabled the origin of animals in marine environments, followed by their persistence in aerobic marine habitats ever since. However, recent studies of redox proxies (e.
View Article and Find Full Text PDFMar Environ Res
October 2025
Frontiers Science Center for Deep Ocean Multispheres and Earth System, and Key Laboratory of Marine Chemistry Theory and Technology, Ministry of Education, China; College of Chemistry and Chemical Engineering, Ocean University of China, Qingdao, 266100, China; Laboratory for Marine Ecology and Envir
This study investigated the sorption characteristics of methylphosphonic acid (MPn) on marine sediments, focusing on the effects of sediment composition and environmental factors. The results indicated that MPn showed good stability on sediment samples and physical process was the main fraction for MPn sorption. Light fraction organic matter (LFOM) significantly enhanced the sorption ability of the sediments.
View Article and Find Full Text PDFNat Commun
August 2025
Department of Earth and Atmospheric Sciences, University of Alberta, Edmonton, AB, Canada.
The Sturtian and Marinoan glaciations shaped Neoproterozoic palaeoenvironmental evolution. While methane emission likely intensified the Marinoan greenhouse effect, its role during the Sturtian glaciation-coinciding with widespread iron formations (IFs)-remains poorly understood. Here, we analysed bio-essential metals (Ni, Co, Zn), rare earth elements and yttrium (REY), Fe (δFe) and Ni (δNi) isotopes in hematite and magnetite, alongside bulk-rock and in-situ C isotopes of Mn-rich carbonates from five well-preserved Sturtian-aged IFs in South China.
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