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基于土壤特征和不同方法评估巴西破碎化大西洋森林(BAF)土壤中的碳储量。

Evaluating carbon stocks in soils of fragmented Brazilian Atlantic Forests (BAF) based on soil features and different methodologies.

机构信息

Department of Forest, Soil and Environmental Sciences, College of Agricultural Sciences, São Paulo State University-UNESP, Botucatu, SP, 18610-034, Brazil.

Federal Institute of Education, Science and Technology of Goiás, Center of Reference in Research and Innovation - CITELAB IFG, Goiânia, GO, 74594111, Brazil.

出版信息

Sci Rep. 2024 May 1;14(1):10007. doi: 10.1038/s41598-024-60629-y.

DOI:10.1038/s41598-024-60629-y
PMID:38693157
原文链接:https://pmc.ncbi.nlm.nih.gov/articles/PMC11063065/
Abstract

Brazil's Atlantic Forest (BAF) is a highly fragmented, strategic environmental and socio-economic region that represents the fourth biodiversity hotspot while also producing many commodities that are exported globally. Human disturbance plays a pivotal role as a driver of BAF's soil dynamics and behaviors. The soils under Late Primary and Secondary Semideciduous Seasonal Forests (LPSF and LSSF) were characterized by high to moderate resilience, with improved chemical properties as human disturbance decreased. The Transitional Forest to Cerrado (TFC) had the worst soil conditions. Disturbed Primary and Secondary Semideciduous Seasonal Forests (DPSF and DSSF) represent a transitional stage between LPSF/LSSF and TFC. Accordingly, SOCs stocks increased from TFC << DPSF, DSSF < LPSF, LSSF. In BAF soils, to avoid unreliable data, SOCs measurements should be (i) conducted to at least 1 m soil depth and (ii) quantified with a CHN analyzer. Human disturbance strongly affected the positive feedback between vegetation succession, SOCs, and soil nutrition. Soil development decreased as human disturbance increased, thus negatively affecting SOCs. Soils in the BAF require a long time to recover after the end of human disturbance, thus suggesting that preservation strategies should be prioritized in remnant BAF fragments.

摘要

巴西大西洋森林(BAF)是一个高度破碎的、具有战略意义的环境和社会经济区域,它是第四大生物多样性热点,同时也是许多全球出口商品的产地。人类干扰是驱动 BAF 土壤动态和行为的关键因素。在晚原生和次生季节性半落叶林(LPSF 和 LSSF)下的土壤具有高到中等的恢复力,随着人类干扰的减少,土壤化学性质得到改善。过渡林到塞拉多(TFC)的土壤条件最差。受干扰的原生和次生季节性半落叶林(DPSF 和 DSSF)代表了 LPSF/LSSF 和 TFC 之间的过渡阶段。因此,SOCs 储量从 TFC<DPSF、DSSF<LPSF、LSSF 逐渐增加。在 BAF 土壤中,为了避免不可靠的数据,SOCs 的测量应该(i)至少进行到 1 米的土壤深度,(ii)用 CHN 分析仪进行量化。人类干扰强烈影响了植被演替、SOCs 和土壤养分之间的正反馈。随着人类干扰的增加,土壤发育减少,从而对 SOCs 产生负面影响。BAF 的土壤在人类干扰结束后需要很长时间才能恢复,因此建议在剩余的 BAF 碎片中优先考虑保护策略。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b546/11063065/c97cec32a166/41598_2024_60629_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b546/11063065/5233a6bef1f7/41598_2024_60629_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b546/11063065/b4599a3a1501/41598_2024_60629_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b546/11063065/c97cec32a166/41598_2024_60629_Fig3_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b546/11063065/5233a6bef1f7/41598_2024_60629_Fig1_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b546/11063065/b4599a3a1501/41598_2024_60629_Fig2_HTML.jpg
https://cdn.ncbi.nlm.nih.gov/pmc/blobs/b546/11063065/c97cec32a166/41598_2024_60629_Fig3_HTML.jpg

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