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Tidal marshes store large amounts of organic carbon in their soils. Field data quantifying soil organic carbon (SOC) stocks provide an important resource for researchers, natural resource managers, and policy-makers working towards the protection, restoration, and valuation of these ecosystems. We collated a global dataset of tidal marsh soil organic carbon (MarSOC) from 99 studies that includes location, soil depth, site name, dry bulk density, SOC, and/or soil organic matter (SOM). The MarSOC dataset includes 17,454 data points from 2,329 unique locations, and 29 countries. We generated a general transfer function for the conversion of SOM to SOC. Using this data we estimated a median (± median absolute deviation) value of 79.2 ± 38.1 Mg SOC ha in the top 30 cm and 231 ± 134 Mg SOC ha in the top 1 m of tidal marsh soils globally. This data can serve as a basis for future work, and may contribute to incorporation of tidal marsh ecosystems into climate change mitigation and adaptation strategies and policies.
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http://dx.doi.org/10.1038/s41597-023-02633-x | DOI Listing |
Environ Monit Assess
September 2025
Institute of Environmental Studies, Kurukshetra University, Kurukshetra, Haryana, 136119, India.
India produces an estimated 6.38 million tons of surplus sugarcane trash annually. When burned in fields, this trash emits approximately 12,948 kg CO equivalent greenhouse gases per hectare and causes nutrient losses (41 kg ha nitrogen, 5.
View Article and Find Full Text PDFFront Mol Biosci
August 2025
Department of Environmental Science, University of Arizona, Tucson, AZ, United States.
Introduction: Peatlands store up to a third of global soil carbon, and in high latitudes their litter inputs are increasing and changing in composition under climate change. Although litter significantly influences peatland carbon and nutrient dynamics by changing the overall lability of peatland organic matter, the physicochemical mechanisms of this impact-and thus its full scope-remain poorly understood.
Methods: We applied multimodal metabolomics (UPLC-HRMS, H NMR) paired with C Stable Isotope-Assisted Metabolomics (SIAM) to track litter carbon and its potential priming effects on both existing soil organic matter and carbon gas emissions.
Front Plant Sci
August 2025
Department Soil Science and Environmental Analyses, Institute of Soil Science and Plant Cultivation-State Research Institute, Puławy, Poland.
Introduction: Soil dissolved organic matter (DOM) regulates nutrient cycling and carbon sequestration, yet how cropping systems (rotation vs. monoculture) shape the vertical distribution and molecular traits of DOM remains unclear.
Methods: We leveraged a long-term experiment (est.
Front Plant Sci
August 2025
Institute of Biotechnology, Inner Mongolia Tongliao Agricultural and Animal Husbandry Academy, Tongliao, China.
Introduction: Straw return combined with rational nitrogen (N) fertilization plays a critical role in coordinating the transformation of soil organic carbon and nitrogen availability, thereby improving nitrogen use efficiency (NUE), crop yield, and soil fertility. However, the dynamics of soil carbon and nitrogen fractions under straw return with varying N inputs, and their specific contributions to NUE and yield, remain unclear.
Methods: A three-year split-plot field experiment was conducted in the Tumochuan Plain Irrigation District.
Acta Crystallogr E Crystallogr Commun
September 2025
Department of Chemistry, University of Gondar, PO Box 196, Gondar, Ethiopia.
The conformation of the title mol-ecule, CHClNO, is maintained by intra-molecular N-H⋯O, C-H⋯O, and C-H⋯Cl inter-actions, creating (6), (5), and (6) motifs, respectively. In the crystal, inter-molecular N-H⋯O, C-H⋯O, and C-H⋯Cl inter-actions connect the mol-ecules, forming a three-dimensional network. Additionally, the mol-ecules are linked by C-H⋯π inter-actions, forming layers parallel to the (002) plane.
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