在碳酸盐化学中，远洋钙化物沿海洋表面梯度扩散

IF 16.1 1区地球科学 Q1 GEOSCIENCES, MULTIDISCIPLINARY

Nature Geoscience Pub Date : 2025-02-12 DOI:10.1038/s41561-025-01646-y

引用次数: 0

摘要

海洋表面区域的自然梯度表明，海洋碱度增强预估的碳酸盐化学变化可能促进钙化浮游植物的增殖。这种转变将增加碱度汇，从而降低作为二氧化碳去除方法的海洋碱度增强的效率。

本文章由计算机程序翻译，如有差异，请以英文原文为准。

Pelagic calcifier proliferation along surface ocean gradients in carbonate chemistry

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Pelagic calcifier proliferation along surface ocean gradients in carbonate chemistry

Natural gradients across surface ocean regions show that changes in carbonate chemistry projected for ocean alkalinity enhancement could promote the proliferation of calcifying phytoplankton. This shift would increase an alkalinity sink, thus reducing the efficiency of ocean alkalinity enhancement as a CO2 removal method.

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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.