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1.
Nature ; 629(8010): 105-113, 2024 May.
Artigo em Inglês | MEDLINE | ID: mdl-38632407

RESUMO

Arctic and alpine tundra ecosystems are large reservoirs of organic carbon1,2. Climate warming may stimulate ecosystem respiration and release carbon into the atmosphere3,4. The magnitude and persistency of this stimulation and the environmental mechanisms that drive its variation remain uncertain5-7. This hampers the accuracy of global land carbon-climate feedback projections7,8. Here we synthesize 136 datasets from 56 open-top chamber in situ warming experiments located at 28 arctic and alpine tundra sites which have been running for less than 1 year up to 25 years. We show that a mean rise of 1.4 °C [confidence interval (CI) 0.9-2.0 °C] in air and 0.4 °C [CI 0.2-0.7 °C] in soil temperature results in an increase in growing season ecosystem respiration by 30% [CI 22-38%] (n = 136). Our findings indicate that the stimulation of ecosystem respiration was due to increases in both plant-related and microbial respiration (n = 9) and continued for at least 25 years (n = 136). The magnitude of the warming effects on respiration was driven by variation in warming-induced changes in local soil conditions, that is, changes in total nitrogen concentration and pH and by context-dependent spatial variation in these conditions, in particular total nitrogen concentration and the carbon:nitrogen ratio. Tundra sites with stronger nitrogen limitations and sites in which warming had stimulated plant and microbial nutrient turnover seemed particularly sensitive in their respiration response to warming. The results highlight the importance of local soil conditions and warming-induced changes therein for future climatic impacts on respiration.


Assuntos
Respiração Celular , Ecossistema , Aquecimento Global , Tundra , Regiões Árticas , Carbono/metabolismo , Carbono/análise , Ciclo do Carbono , Conjuntos de Dados como Assunto , Concentração de Íons de Hidrogênio , Nitrogênio/metabolismo , Nitrogênio/análise , Plantas/metabolismo , Estações do Ano , Solo/química , Microbiologia do Solo , Temperatura , Fatores de Tempo
2.
Proc Natl Acad Sci U S A ; 115(5): 833-835, 2018 01 30.
Artigo em Inglês | MEDLINE | ID: mdl-29330330
3.
Ecol Evol ; 3(11): 3804-23, 2013 Oct.
Artigo em Inglês | MEDLINE | ID: mdl-24198941

RESUMO

Private forests harbor considerable biodiversity, however, they are under greater threat than reserved areas, particularly from urbanization, agriculture, and intense exploitation for timber and fuel wood. The extent to which they may act as habitats for biodiversity and how level of protection impacts trends in biodiversity and forest structure over time remain underresearched. We contribute to filling this research gap by resampling a unique data set, a detailed survey from 1990 of 22 forests fragments of different ownership status and level of protection near Kampala, Uganda. Eleven of the 22 fragments were lost over 20 years, and six of the remnants reduced in size. Forest structure and composition also showed dramatic changes, with six of the remnant fragments showing high temporal species turnover. Species richness increased in four of the remaining forests over the resample period. Forest ownership affected the fate of the forests, with higher loss in privately owned forests. Our study demonstrates that ownership affects the fate of forest fragments, with private forests having both higher rates of area loss, and of structural and compositional change within the remaining fragments. Still, the private forests contribute to the total forest area, and they harbor biodiversity including IUCN "vulnerable" and "endangered" species. This indicates the conservation value of the fragments and suggests that they should be taken into account in forest conservation and restoration.

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