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估算飓风对佛罗里达州西南部红树林湿地碳储存的影响。

Estimating the Effects of a Hurricane on Carbon Storage in Mangrove Wetlands in Southwest Florida.

作者信息

Griffiths Lauren N, Mitsch William J

机构信息

Everglades Wetland Research Park, The Water School, Florida Gulf Coast University, 4940 Bayshore Drive, Naples, FL 34112, USA.

School of Geosciences, University of South Florida, 4202 E. Fowler Avenue, Tampa, FL 33620, USA.

出版信息

Plants (Basel). 2021 Aug 23;10(8):1749. doi: 10.3390/plants10081749.

Abstract

Tropical and subtropical mangrove swamps, under normal conditions, can sequester large amounts of carbon in their soils but as coastal wetlands, they are prone to hurricane disturbances. This study adds to the understanding of carbon storage capabilities of mangrove wetlands and explores how these capacities might change within the scope of a changing storm climate. In September 2017, Naples Bay, FL, USA (28°5' N, 81°47' W) encountered a direct hit from hurricane Irma, a Saffir-Simpson category 3 storm. By comparing carbon storage, forest community structure, and aboveground productivity collected in 2013 and in 2019, we estimated the effects of hurricane Irma on mangrove functions. Aboveground biomass increased during the study period at a rate of approximately 0.72 kg m yr, significantly less than the average found in undisturbed mangrove forests. Soil carbon storage decreased at all study sites. On average, 2.7 kg-C m was lost in the top 20 cm between sample collections. Carbon loss in belowground pools could point to a feedback of mangrove swamps on climate change as they lose their ability to store carbon and increase net atmospheric carbon. Nevertheless, mangrove swamps remain resilient to tropical storms in the long term and can recover their carbon storage capacity in the years following a storm.

摘要

在正常情况下,热带和亚热带红树林沼泽能够在其土壤中固存大量碳,但作为沿海湿地,它们容易受到飓风干扰。本研究增进了对红树林湿地碳储存能力的理解,并探讨了在不断变化的风暴气候范围内这些能力可能如何变化。2017年9月,美国佛罗里达州那不勒斯湾(北纬28°5′,西经81°47′)遭受了3级萨菲尔-辛普森飓风“厄玛”的直接袭击。通过比较2013年和2019年收集的碳储存、森林群落结构和地上生产力数据,我们估算了“厄玛”飓风对红树林功能的影响。在研究期间,地上生物量以每年约0.72千克/平方米的速度增加,显著低于未受干扰的红树林森林中的平均水平。所有研究地点的土壤碳储存都减少了。在样本采集期间,平均每平方米前20厘米的土层中损失了2.7千克碳。地下碳库的损失可能表明红树林沼泽对气候变化的一种反馈,因为它们失去了储存碳的能力,增加了大气中的净碳含量。尽管如此,从长期来看,红树林沼泽对热带风暴仍具有恢复力,并且在风暴过后的几年内能够恢复其碳储存能力。

https://cdn.ncbi.nlm.nih.gov/pmc/blobs/0928/8398776/726f06dfdb3f/plants-10-01749-g001.jpg

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