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Coastal and intertidal habitats are at the forefront of anthropogenic influence and environmental change. The species occupying these habitats are adapted to a world of extremes, which may render them robust to the changing climate or more vulnerable if they are at their physiological limits. We characterized the diurnal, seasonal and interannual patterns of flux in biogeochemistry across an intertidal gradient on a temperate sandstone platform in eastern Australia over 6 years (2009-2015) and present a synthesis of our current understanding of this habitat in context with global change. We used rock pools as natural mesocosms to determine biogeochemistry dynamics and patterns of eco-stress experienced by resident biota. In situ measurements and discrete water samples were collected night and day during neap low tide events to capture diurnal biogeochemistry cycles. Calculation of pH using total alkalinity (TA) and dissolved inorganic carbon (DIC) revealed that the mid-intertidal habitat exhibited the greatest flux over the years (pH 7.52-8.87), and over a single tidal cycle (1.11 pH units), while the low-intertidal (pH 7.82-8.30) and subtidal (pH 7.87-8.30) were less variable. Temperature flux was also greatest in the mid-intertidal (8.0-34.5°C) and over a single tidal event (14°C range), as typical of temperate rocky shores. Mean TA and DIC increased at night and decreased during the day, with the most extreme conditions measured in the mid-intertidal owing to prolonged emersion periods. Temporal sampling revealed that net ecosystem calcification and production were highest during the day and lowest at night, particularly in the mid-intertidal. Characterization of biogeochemical fluctuations in a world of extremes demonstrates the variable conditions that intertidal biota routinely experience and highlight potential microhabitat-specific vulnerabilities and climate change refugia.
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http://dx.doi.org/10.1111/gcb.15103 | DOI Listing |
Water Res
August 2025
College of Environmental Science and Engineering, Hunan University, Changsha 410082, PR China; Key Laboratory of Environmental Biology and Pollution Control (Hunan University), Ministry of Education, Changsha 410082, PR China.
Lakes serve as critical regulators of biogeochemical processes, acting as hotspots for nitrous oxide (NO) emissions while simultaneously retaining substantial phosphorus loads. However, the role of total phosphorus (TP) in shaping NO dynamics remains poorly understood. Here, we investigated TP-mediated changes in NO concentrations in Dongting Lake, China, using a classification framework based on national water quality standards, validated with the GRiMe dataset and machine learning approaches.
View Article and Find Full Text PDFNature
August 2025
International Center for Isotope Effects Research, State Key Laboratory of Critical Earth Material Cycling and Mineral Deposits, School of Earth Sciences and Engineering, Nanjing University, Nanjing, China.
Earth's surface underwent stepwise oxygenation before persistently reaching modern levels late in its history, but the details of this transition remain unclear. Here we present a high-resolution 2.5-Gyr record of mass-independent oxygen isotopes in sedimentary sulfate (Δ'O), a proxy linked to the atmospheric partial pressure of O ( ).
View Article and Find Full Text PDFMar Pollut Bull
August 2025
Centro de Estudios Avanzados de Blanes, Consejo Superior de Investigaciones Científicas (CEAB-CSIC), Blanes, Spain; School of Science, Centre for Marine Ecosystems Research, Edith Cowan University, Joondalup, WA, Australia.
Current knowledge of long-term mercury (Hg) deposition is predominantly based on studies from the Northern Hemisphere, leading to a geographical bias in the comprehension of the global Hg cycle. Aiming to contribute to fill this knowledge gap, our study presents a high-resolution Hg record of a seagrass Posidonia australis sedimentary archive encompassing the last 3300 years in the Waychinicup estuary (Western Australia, WA). This setting is an ideal site for studying the natural Hg cycle, as it is located in the southwest of the state, outside the prevailing wind patterns that transport emissions from major Hg sources.
View Article and Find Full Text PDFGlob Chang Biol
August 2025
State Key Laboratory of Forage Breeding-By-Design and Utilization, Key Laboratory of Vegetation and Environmental Change, Institute of Botany, Chinese Academy of Sciences, Beijing, China.
Litter decomposition is a critical biogeochemical process for carbon and nutrient cycling in terrestrial ecosystems. Ultraviolet (UV) radiation has been recognized to accelerate litter-derived C release in arid and semi-arid ecosystems; yet its spatial controls on determining the regional pattern of litter decomposition are poorly explored. Moreover, the limited understanding of how UV radiation interacts with traditional decomposition drivers, such as climate and litter quality, significantly restricts our ability to accurately quantify the contribution of UV-driven photodegradation to large-scale carbon turnover.
View Article and Find Full Text PDFBioresour Technol
December 2025
Dalian Polytechnic University, Dalian 116034, China. Electronic address:
Microbial nitrogen metabolism serves as the core driver of biogeochemical cycles, governing over 90% of global nitrogen transformations through enzymatic cascades. Its core regulatory mechanisms encompass a three-tiered system-nitrogen source perception, signal transduction, and systemic network control-enabling dynamic adaptation to nitrogen fluctuations while confronting key challenges including metabolic crosstalk complexity between carbon and nitrogen pathways and energy co-integration. Recent technological breakthroughs include cryo-electron microscopy elucidating the dynamic structures of key enzymes and artificial intelligence-driven multi-omics revealing metabolic network interactions.
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