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Fire in the Earth System

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TLDR
What is known and what is needed to develop a holistic understanding of the role of fire in the Earth system are reviewed, particularly in view of the pervasive impact of fires and the likelihood that they will become increasingly difficult to control as climate changes.
Abstract
Fire is a worldwide phenomenon that appears in the geological record soon after the appearance of terrestrial plants. Fire influences global ecosystem patterns and processes, including vegetation distribution and structure, the carbon cycle, and climate. Although humans and fire have always coexisted, our capacity to manage fire remains imperfect and may become more difficult in the future as climate change alters fire regimes. This risk is difficult to assess, however, because fires are still poorly represented in global models. Here, we discuss some of the most important issues involved in developing a better understanding of the role of fire in the Earth system.

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Citations
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Satellite-based assessment of climate controls on US burned area

TL;DR: In this article, the authors conducted the first national assessment of climate controls on US fire activity using two satellite-based estimates of monthly burned area (BA), the Global Fire Emissions Database (GFED, 1997-2010) and Monitoring Trends in Burn Severity (MTBS, 1984-2009) BA products.
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Mega fire emissions in Siberia: potential supply of bioavailable iron from forests to the ocean

TL;DR: In this article, the potential contribution of forest fires to the deposition of bioavailable iron (Fe) into the ocean is highlighted, with a focus on mega fires in eastern Siberia.
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A 350‐million‐year legacy of fire adaptation among conifers

TL;DR: It is concluded that many early conifers were serotinous in response to intense crown fires, indicating that fire may have had a major impact on the evolution of plant traits as far back as 350 Ma.
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Rethinking infiltration in wildfire‐affected soils

TL;DR: In this paper, the fundamental physics of infiltration in wildfire-affected soils is compared to unburned soils (e.g., Imeson et al., 1992, Moody et al, 2009, Moody and Ebel, 2012), which can provide estimates of peak discharge, start of runoff, time to peak and total runoff for hydroclimatic scenarios after wildfire.
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Mobilizing the past to shape a better Anthropocene.

TL;DR: In this paper, the authors argue that information from the past has a valuable role to play in enhancing the sustainability and resilience of our societies and highlight the ways that past data can be mobilized for a variety of efforts, from supporting conservation to increasing agricultural sustainability and food security.
References
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疟原虫var基因转换速率变化导致抗原变异[英]/Paul H, Robert P, Christodoulou Z, et al//Proc Natl Acad Sci U S A

宁北芳, +1 more
TL;DR: PfPMP1)与感染红细胞、树突状组胞以及胎盘的单个或多个受体作用,在黏附及免疫逃避中起关键的作�ly.
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Warming and Earlier Spring Increase Western U.S. Forest Wildfire Activity

TL;DR: It is shown that large wildfire activity increased suddenly and markedly in the mid-1980s, with higher large-wildfire frequency, longer wildfire durations, and longer wildfire seasons.
Journal ArticleDOI

Forests and Climate Change: Forcings, Feedbacks, and the Climate Benefits of Forests

TL;DR: Interdisciplinary science that integrates knowledge of the many interacting climate services of forests with the impacts of global change is necessary to identify and understand as yet unexplored feedbacks in the Earth system and the potential of forests to mitigate climate change.
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