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Temperature responses of ecosystem respiration 生态系统呼吸的温度响应
Pub Date : 2024-07-16 DOI: 10.1038/s43017-024-00569-3
Shuli Niu, Weinan Chen, Lìyǐn L. Liáng, Carlos A. Sierra, Jianyang Xia, Song Wang, Mary Heskel, Kaizad F. Patel, Ben Bond-Lamberty, Jinsong Wang, Gabriel Yvon-Durocher, Miko U. F. Kirschbaum, Owen K. Atkin, Yuanyuan Huang, Guirui Yu, Yiqi Luo
Terrestrial ecosystems release ~106–130 PgC yr–1 into the atmosphere through respiration, counterbalancing photosynthetic carbon uptake and determining the strength of the land carbon sink. The effect of anthropogenic warming on the land carbon sink will depend on the temperature response of respiration. In this Review, we explore the relationships between temperature and ecosystem respiration from experimental and observational data at leaf, microbial, ecosystem and global scales. Contrary to the assumed monotonic increase in respiration with increasing temperature derived from Earth system models, empirical findings indicate a unimodal temperature response with a peak in respiration at an optimal temperature (Topt). This unimodality is observed across a range of organization levels with Topt values of 40–60 °C at the leaf and plant level, 11–46 °C at a microbial level and 6.5–33.3 °C at the global scale. Various mechanisms contribute to this unimodal pattern including enzyme deactivation, the thermodynamics of enzyme-catalysed reactions and changes in temperature-dependent factors such as soil moisture, nutrient availability and vegetation physiology. Incorporating the unimodality of these observed temperature responses of ecosystem respiration into Earth system models could facilitate attribution studies to identify the mechanisms responsible for the peaked response and increase the accuracy of carbon sequestration predictions. The future of the land carbon sink depends on the temperature response of ecosystem respiration. This Review explores observational and experimental evidence for a unimodal temperature response of respiration and the implications for carbon sequestration predictions.
陆地生态系统每年通过呼吸作用向大气释放约 106-130 PgC,抵消光合作用的碳吸收,并决定陆地碳汇的强度。人为变暖对陆地碳汇的影响将取决于呼吸作用的温度响应。在本综述中,我们将从叶片、微生物、生态系统和全球尺度的实验和观测数据中探讨温度与生态系统呼吸作用之间的关系。与地球系统模型假定的呼吸作用随温度升高而单调增加的情况相反,实证研究结果表明,温度反应具有单模态性,呼吸作用在最佳温度(Topt)达到峰值。在一系列组织水平上都可以观察到这种单模性,叶片和植物水平的 Topt 值为 40-60℃,微生物水平的 Topt 值为 11-46℃,全球范围的 Topt 值为 6.5-33.3℃。造成这种单模态模式的机制多种多样,包括酶失活、酶催化反应的热力学以及土壤湿度、养分供应和植被生理等温度相关因素的变化。将观测到的生态系统呼吸的温度响应的单模性纳入地球系统模型,可促进归因研究,以确定峰值响应的机制,并提高固碳预测的准确性。陆地碳汇的未来取决于生态系统呼吸的温度响应。本综述探讨了呼吸作用单峰温度响应的观测和实验证据及其对固碳预测的影响。
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引用次数: 0
The energy transition needs subsurface geoscience 能源转型需要地下地球科学
Pub Date : 2024-07-11 DOI: 10.1038/s43017-024-00579-1
The switch to a low-carbon economy is heavily reliant on mining, geothermal energy and geological storage. Subsurface geoscientists are critically needed to responsibly source, manage and refine these operations while minimizing environmental and social impacts.
向低碳经济的转变在很大程度上依赖于采矿、地热能源和地质储存。我们急需地下地球科学家来负责任地寻找、管理和完善这些业务,同时最大限度地减少对环境和社会的影响。
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引用次数: 0
Digital ice core imaging to reveal past climate changes 数字冰芯成像揭示过去的气候变化
Pub Date : 2024-07-04 DOI: 10.1038/s43017-024-00575-5
Rahul Dey
Rahul Dey describes how high-resolution digital imaging of ice core layers can be used to infer paleoclimatic changes.
Rahul Dey 介绍了如何利用冰芯层的高分辨率数字成像来推断古气候变化。
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引用次数: 0
Author Correction: Monitoring, trends and impacts of light pollution 作者更正:光污染的监测、趋势和影响
Pub Date : 2024-07-03 DOI: 10.1038/s43017-024-00577-3
Hector Linares Arroyo, Angela Abascal, Tobias Degen, Martin Aubé, Brian R. Espey, Geza Gyuk, Franz Hölker, Andreas Jechow, Monika Kuffer, Alejandro Sánchez de Miguel, Alexandre Simoneau, Ken Walczak, Christopher C. M. Kyba
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引用次数: 0
Achieving the Kunming–Montreal global biodiversity targets for blue carbon ecosystems 实现昆明-蒙特利尔蓝碳生态系统全球生物多样性目标
Pub Date : 2024-07-02 DOI: 10.1038/s43017-024-00566-6
Chuancheng Fu, Alexandra Steckbauer, Hugo Mann, Carlos M. Duarte
The Kunming–Montreal Global Biodiversity Framework (KM-GBF) provides a major impetus for the restoration and conservation of blue carbon ecosystems to address the biodiversity and climate crises. In this Perspective, we translate the KM-GBF targets for blue carbon ecosystems into quantitative metrics, outline action that must be taken to achieve these goals and quantify the associated climate benefits. To achieve the KM-GBF targets, net mangrove, saltmarsh and seagrass losses of 187–190 km2, 76–126 km2 and 3,068–3,597 km2, respectively, must be avoided annually from 2030 onwards and 23,693–24,369 km2, 10,467–17,296 km2 and 90,601–106,215 km2 of these ecosystems must be restored. Achieving the KM-GBF targets would contribute 2.8% of the reduction of carbon emissions needed to limit anthropogenic warming to 2 °C by 2030. However, the cost of achieving the targets (US$520.1 billion yr–1) far exceeds the amount pledged ($200 billion yr–1) for all ecosystems. Thus, research is needed to develop cost-effective restoration and conservation technologies, along with innovative financial models to incentivize investments in nature. Additionally, blue carbon actions must be embedded within National Biodiversity Strategies and Action Plans to ensure that the targets are met. Degradation and loss of blue carbon ecosystems contributes to climate change, weakens coastal protection and threatens biodiversity. This Perspective outlines the actions required to achieve goals to restore and protect these ecosystems.
昆明-蒙特利尔全球生物多样性框架(KM-GBF)为恢复和保护蓝碳生态系统以应对生物多样性和气候危机提供了重要动力。在本《视角》中,我们将 KM-GBF 的蓝碳生态系统目标转化为量化指标,概述实现这些目标必须采取的行动,并量化相关的气候效益。要实现知识管理-全球蓝碳论坛目标,从 2030 年起,每年必须避免红树林、盐沼和海草的净损失分别为 187-190 平方公里、76-126 平方公里和 3068-3597 平方公里,必须恢复这些生态系统的面积分别为 23693-24369 平方公里、10467-17296 平方公里和 90601-106215 平方公里。实现知识管理-全球生物多样性框架目标将有助于减少 2.8%的碳排放量,从而到 2030 年将人为变暖限制在 2 °C。然而,实现这些目标的成本(5,201 亿美元/年-1)远远超过了对所有生态系统的承诺金额(2,000 亿美元/年-1)。因此,需要研究开发具有成本效益的恢复和保护技术,同时采用创新的金融模式来激励对自然的投资。此外,蓝碳行动必须纳入国家生物多样性战略和行动计划,以确保实现目标。
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引用次数: 0
Challenging perceptions of underground hydrogen storage 挑战对地下储氢的认识
Pub Date : 2024-07-02 DOI: 10.1038/s43017-024-00572-8
Katriona Edlmann
Underground hydrogen storage (UHS) will be an essential part of the energy transition. Over 45 pilot projects are underway to reduce the technical and regulatory risks of UHS, but negative perceptions must be addressed to ensure that hydrogen’s role in achieving net zero targets can be realized.
地下储氢(UHS)将成为能源转型的重要组成部分。超过 45 个试点项目正在进行中,以降低地下储氢系统的技术和监管风险,但必须消除负面看法,以确保氢能在实现净零目标方面发挥作用。
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引用次数: 0
Political obstacles to carbon capture and storage for carbon removal 碳捕集与碳封存除碳的政治障碍
Pub Date : 2024-07-02 DOI: 10.1038/s43017-024-00574-6
Nils Markusson
Using carbon dioxide capture and storage (CCS) for carbon removal is crucial to climate policy, but implementation at scale is at risk owing to political obstacles. Climate policies must avoid relying on empty promises of CCS for carbon removal without necessary financial resourcing and support emissions reductions separately from carbon removal.
利用二氧化碳捕集与封存(CCS)进行碳清除对气候政策至关重要,但由于政治障碍,大规模实施面临风险。气候政策必须避免在没有必要财政资源的情况下依赖空洞的 CCS 碳清除承诺,并在碳清除之外单独支持减排。
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引用次数: 0
Using drones to sample volcanic plumes 使用无人机对火山羽流进行采样
Pub Date : 2024-06-26 DOI: 10.1038/s43017-024-00570-w
Laura Wainman
Laura Wainman explains how drones can be used to sample the composition and dynamics of volcanic plumes.
劳拉-温曼(Laura Wainman)解释了如何利用无人机对火山羽流的成分和动态进行采样。
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引用次数: 0
Phase-sensitive radar measurements of glacial processes 对冰川过程进行相位敏感的雷达测量
Pub Date : 2024-06-19 DOI: 10.1038/s43017-024-00571-9
Falk M. Oraschewski
Falk Oraschewski describes how phase-sensitive radio echo sounding can be used to measure melting at the base of ice shelves and englacial ice crystal orientations.
Falk Oraschewski 介绍了如何利用相位敏感无线电回声探测来测量冰架底部的融化和冰川冰晶的方向。
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引用次数: 0
From academia to a career in programme management 从学术界到计划管理职业生涯
Pub Date : 2024-06-17 DOI: 10.1038/s43017-024-00568-4
Graham Simpkins, Allen Pope
To explore career opportunities outside of academia, Nature Reviews Earth & Environment interviewed Allen Pope about their career path from research scientist to programme director at the U.S. National Science Foundation.
为了探索学术界以外的职业机会,《自然-地球与环境》杂志采访了艾伦-波普,了解他们从研究科学家到美国国家科学基金会项目主任的职业道路。
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引用次数: 0
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