Sulfur cycling in thawing permafrost landscapes

IF 16.1 1区地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY

Nature Geoscience Pub Date : 2025-10-09 DOI:10.1038/s41561-025-01804-2

Clement P. Bataille, Elliott K. Skierszkan

引用次数: 0

Abstract

A negative sulfur isotope excursion occurred across Eurasia during the last deglaciation. An analysis suggests thawing permafrost might be responsible.

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永久冻土融化中的硫循环

在最后一次消冰期间，欧亚大陆发生了负硫同位素偏移。一项分析表明，冻土融化可能是罪魁祸首。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

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来源期刊

Nature Geoscience 地学-地球科学综合

CiteScore

26.70

自引率

1.60%

发文量

187

审稿时长

3.3 months

期刊介绍： Nature Geoscience is a monthly interdisciplinary journal that gathers top-tier research spanning Earth Sciences and related fields. The journal covers all geoscience disciplines, including fieldwork, modeling, and theoretical studies. Topics include atmospheric science, biogeochemistry, climate science, geobiology, geochemistry, geoinformatics, remote sensing, geology, geomagnetism, paleomagnetism, geomorphology, geophysics, glaciology, hydrology, limnology, mineralogy, oceanography, paleontology, paleoclimatology, paleoceanography, petrology, planetary science, seismology, space physics, tectonics, and volcanology. Nature Geoscience upholds its commitment to publishing significant, high-quality Earth Sciences research through fair, rapid, and rigorous peer review, overseen by a team of full-time professional editors.