Biogeochemistry, Год журнала: 2022, Номер 157(3), С. 355 - 378
Опубликована: Янв. 17, 2022
Язык: Английский
Biogeochemistry, Год журнала: 2022, Номер 157(3), С. 355 - 378
Опубликована: Янв. 17, 2022
Язык: Английский
Plant and Soil, Год журнала: 2024, Номер 500(1-2), С. 481 - 494
Опубликована: Фев. 14, 2024
Язык: Английский
Процитировано
6The Science of The Total Environment, Год журнала: 2024, Номер 926, С. 171605 - 171605
Опубликована: Март 8, 2024
Язык: Английский
Процитировано
6Journal of Environmental Management, Год журнала: 2023, Номер 349, С. 119480 - 119480
Опубликована: Окт. 31, 2023
Язык: Английский
Процитировано
14Geoderma, Год журнала: 2024, Номер 446, С. 116904 - 116904
Опубликована: Май 7, 2024
The global warming-driven poleward expansion of mangrove habitats (e.g., Avicennia germinans and Rhizophora mangle) into temperate salt marshes Spartina alterniflora Juncus roemerianus) has been shown to alter coastal soil organic carbon (SOC) storage. However, the taxa-specific consequences this vegetation shift on origin size SOC sub-fractions (particulate OC (POC); mineral-associated (MAOC); reactive iron-associated (FeR-MAOC)) remain largely unexplored. In study, we used a particle size-based fractionation method compare quantity δ13C composition bulk each in cores collected from Apalachicola Bay barrier islands Florida, USA, highest latitude where monospecific communities all four aforementioned plants co-occur. Depth-dependent variation clearly showed replacement S. by mangroves, as well reciprocal substitutions J. roemerianus, probably driven changes wetland elevation. Higher burial rates suggested that soils were principally developed deposition. contrast, comparatively lower but higher stocks marsh illustrated subsurface input roots. POC was primarily derived contemporary plant detritus; its concentration (58.8 ± 9.0 % SOC) relative mangroves (38.4 6.0 SOC). MAOC content did not vary across (53.5 10.9 SOC), originated microbially-transformed pre-existing plants. FeR-MAOC essentially absent R. mangle (2.9 3.6 while representing minor fraction three other (7.8 7.0 more like present-day surface plants, highlighting situ formation their active oxidizing rhizospheres.
Язык: Английский
Процитировано
5Journal of Soils and Sediments, Год журнала: 2025, Номер unknown
Опубликована: Янв. 21, 2025
Язык: Английский
Процитировано
0Science China Earth Sciences, Год журнала: 2025, Номер unknown
Опубликована: Март 19, 2025
Язык: Английский
Процитировано
0Applied Soil Ecology, Год журнала: 2025, Номер 209, С. 106058 - 106058
Опубликована: Март 26, 2025
Язык: Английский
Процитировано
0CATENA, Год журнала: 2023, Номер 225, С. 107019 - 107019
Опубликована: Фев. 20, 2023
Язык: Английский
Процитировано
10Biogeosciences, Год журнала: 2023, Номер 20(23), С. 4761 - 4774
Опубликована: Дек. 1, 2023
Abstract. Reactive iron (Fe) oxides are vital for long-term soil or sediment organic carbon (SOC) storage. However, the patterns and drivers of Fe-associated (Fe-OC) over global geographic scales under various ecosystem types remain controversial. Here, we provided a systematic assessment distribution determinants Fe-OC content its contribution to SOC (fFe-OC) by assembling dataset comprising 862 observations from 325 sites in distinct ecosystems. We found that across ecosystems ranged 0 83.3 g kg−1 (fFe-OC % 82.4 %), reflecting high variability pool. contents varied with type being greater wetlands molar ratio / dithionite-extractable Fe (Fed) compared marine terrestrial Furthermore, fFe-OC was significantly lower than other due rich (OC). In contrast climate variables pH, random forest modeling multivariate analysis showed : Fed were predominant predictors ecosystems, whereas primary driver Based on upper estimates storage types, further estimated 83.84 ± 3.8, 172.45 8.74, 24.48 0.87 Pg preserved association wetland, terrestrial, respectively. Taken together, our findings highlighted importance reactive preservation, their controlling factors specific.
Язык: Английский
Процитировано
10Soil and Tillage Research, Год журнала: 2024, Номер 240, С. 106105 - 106105
Опубликована: Апрель 3, 2024
Язык: Английский
Процитировано
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