Mina Bizic, Paul del Giorgio, Sofia Baliña, Yves Prairie, Tonya DelSontro, Alberto Borges
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With this special issue of <i>Limnology and Oceanography Letters</i>, we call for papers that contribute to minimizing the knowledge gap in understanding the spatiotemporal variability of methane emissions across the aquatic continuum and the biological, chemical, and physical processes driving it.</p><p>Surface emissions correspond to the net balance between production and consumption processes and include several biotic and abiotic mechanisms such as diffusion and lateral transport of CH<sub>4</sub> from the sediment; demethylation of organic compounds in oxic environments; photosynthesis, ebullition, and emission through macrophytes; and transport by various organisms. Nevertheless, the contribution of individual mechanisms to the accumulation and emission of methane is not well constrained. For example, the contribution of aerobic and anaerobic methane oxidizers to methane consumption in sediments and deeper layers of the water column at the oxic–anoxic interfaces is well studied. In contrast, in the oxic surface layers of oceans and lakes, this process is less understood with contradicting data regarding the inhibitory effects of light and oxygen on the methane oxidation process. As methane emissions are a result of production, transport, and consumption, it is essential to gain a better understanding of the organisms playing a role in the process as well as the different rates of production and consumption.</p><p>The variability in methane emissions from different types of aquatic systems and across various spatial scales, from ponds to large lakes, streams to rivers, estuaries, and oceans, hinders the generation of large-scale models. Novel methanogenesis processes discovered in the last decade are major contributors to methane emissions, yet there is minimal information on their isotopic signatures. Coupled, these two gaps in knowledge contribute to the large discrepancies between top-down and bottom-up approaches when evaluating the role of aquatic systems in the global methane budget.</p><p>We welcome contributions to this Special Issue addressing methane production, consumption, transport, and emissions from different aquatic bodies. Studies may relate to microbial communities involved in CH<sub>4</sub> cycling, quantification of classic and novel processes and pathways, large-scale spatiotemporal studies, isotopic characterization of novel methane sources, as well as novel methodological approaches to quantify methane emissions from water.</p><p>All contributions to this Special Issue must fit within the scope of <i>Limnology and Oceanography Letters</i> (https://aslopubs.onlinelibrary.wiley.com/journal/23782242) and will be assessed with the same level of rigor as regular journal contributions. Accepted papers will be published online in Early View with a permanent DOI. A Virtual Issue of papers submitted to this Special Issue will be bound and added to the journal website collections page. All articles are Open Access, and the publication cost is US$ 2688 for ASLO members and $3360 for nonmembers. The membership cost is only $30 for students and emeritus scientists, $50 for Early Career Scientists, and no cost for students and Early Career Scientists from developing countries (see: https://www.aslo.org/membership-options-join-and-renew/join/). Waivers and discounts of article publication charges are available to corresponding authors based in low- and lower-middle income countries and locations (details: https://aslopubs.onlinelibrary.wiley.com/hub/journal/23782242/resources/apc#:~:text=The%20journal%20does%20not%20charge%20any%20submission%20fees%20or%20page%20charges). Please note the journal's data publication requirement as described in Cloern (<span>2022</span>).</p><p>To determine suitability of a manuscript to the special issue, please submit a 250–300 words manuscript proposal (presubmission inquiry) by 30 September 2024 to the Editor in Chief of <i>Limnology and Oceanography Letters</i>, James E. Cloern at: <span>[email protected]</span>, who will forward the inquiries to the SI editors for evaluation. 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With this special issue of <i>Limnology and Oceanography Letters</i>, we call for papers that contribute to minimizing the knowledge gap in understanding the spatiotemporal variability of methane emissions across the aquatic continuum and the biological, chemical, and physical processes driving it.</p><p>Surface emissions correspond to the net balance between production and consumption processes and include several biotic and abiotic mechanisms such as diffusion and lateral transport of CH<sub>4</sub> from the sediment; demethylation of organic compounds in oxic environments; photosynthesis, ebullition, and emission through macrophytes; and transport by various organisms. Nevertheless, the contribution of individual mechanisms to the accumulation and emission of methane is not well constrained. For example, the contribution of aerobic and anaerobic methane oxidizers to methane consumption in sediments and deeper layers of the water column at the oxic–anoxic interfaces is well studied. In contrast, in the oxic surface layers of oceans and lakes, this process is less understood with contradicting data regarding the inhibitory effects of light and oxygen on the methane oxidation process. As methane emissions are a result of production, transport, and consumption, it is essential to gain a better understanding of the organisms playing a role in the process as well as the different rates of production and consumption.</p><p>The variability in methane emissions from different types of aquatic systems and across various spatial scales, from ponds to large lakes, streams to rivers, estuaries, and oceans, hinders the generation of large-scale models. Novel methanogenesis processes discovered in the last decade are major contributors to methane emissions, yet there is minimal information on their isotopic signatures. 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引用次数: 0
摘要
我们很高兴地宣布,《湖沼学与海洋学快报》特刊将面向水生环境甲烷排放专题征稿(图1)。淡水、半咸淡水和海洋环境对全球甲烷排放有重大贡献,但这些环境估计值的高度变异性是造成自然来源甲烷排放估计值不确定性的主要原因。在本期《湖沼学与海洋学快报》特刊中,我们呼吁投稿论文,以最大限度地缩小理解水生连续体中甲烷排放的时空变异性以及驱动甲烷排放的生物、化学和物理过程方面的知识差距。地表排放对应于生产和消费过程之间的净平衡,包括几种生物和非生物机制,如沉积物中CH4的扩散和侧向运输;有机化合物在氧环境中的去甲基化;通过大型植物的光合作用、沸腾和释放;以及各种生物体的运输。然而,个别机制对甲烷积累和排放的贡献并没有得到很好的约束。例如,好氧和厌氧甲烷氧化剂对沉积物和缺氧界面水柱深层甲烷消耗的贡献得到了很好的研究。相比之下,在海洋和湖泊的含氧表层,人们对这一过程的了解较少,关于光和氧对甲烷氧化过程的抑制作用的数据相互矛盾。由于甲烷排放是生产、运输和消费的结果,因此有必要更好地了解在这一过程中发挥作用的生物以及不同的生产和消费速度。不同类型水生系统和不同空间尺度(从池塘到大湖、溪流到河流、河口和海洋)甲烷排放的变异性阻碍了大尺度模型的生成。过去十年中发现的新型甲烷生成过程是甲烷排放的主要贡献者,但关于其同位素特征的信息很少。在评估水生系统在全球甲烷收支中的作用时,这两个知识缺口导致了自上而下和自下而上方法之间的巨大差异。我们欢迎本期特刊就不同水生生物的甲烷生产、消费、运输和排放问题发表意见。研究可能涉及参与甲烷循环的微生物群落,经典和新型过程和途径的量化,大规模时空研究,新型甲烷来源的同位素表征,以及量化水中甲烷排放的新方法。本期特刊的所有投稿必须符合《湖沼学与海洋学快报》(https://aslopubs.onlinelibrary.wiley.com/journal/23782242)的范围,并将以与常规期刊投稿相同的严格程度进行评估。被接受的论文将在Early View上在线发表,并附有永久DOI。提交到本期特刊的论文将被绑定并添加到期刊网站收藏页面。所有文章都是开放获取的,ASLO会员的出版费用为2688美元,非会员的出版费用为3360美元。学生和退休科学家的会员费用仅为30美元,早期职业科学家的会员费用为50美元,发展中国家的学生和早期职业科学家的会员费用为免费(见:https://www.aslo.org/membership-options-join-and-renew/join/)。低收入和中低收入国家和地区的通讯作者可获得文章出版费用的豁免和折扣(详细信息:https://aslopubs.onlinelibrary.wiley.com/hub/journal/23782242/resources/apc#:~:text=The%20journal%20does%20not%20charge%20any%20submission%20fees%20or%20page%20charges)。请注意期刊的数据发表要求,如Cloern(2022)所述。为了确定稿件是否适合特刊,请在2024年9月30日之前向《湖泊学与海洋学快报》主编James E. Cloern提交一份250-300字的稿件建议(投稿前询问):[email protected],他将把询问转交给SI编辑进行评估。投稿截止日期为2025年6月30日。
Call for Proposals: Special Issue of Limnology and Oceanography Letters: Methane in freshwater, brackish, and marine environments
We are pleased to announce a call for papers for a special issue of Limnology and Oceanography Letters focusing on methane emissions from aquatic environments (Fig. 1).
Freshwater, brackish, and marine environments significantly contribute to global methane emissions, but the high degree of variability in estimates from these environments is largely responsible for the uncertainty in estimates of methane emissions from natural sources. With this special issue of Limnology and Oceanography Letters, we call for papers that contribute to minimizing the knowledge gap in understanding the spatiotemporal variability of methane emissions across the aquatic continuum and the biological, chemical, and physical processes driving it.
Surface emissions correspond to the net balance between production and consumption processes and include several biotic and abiotic mechanisms such as diffusion and lateral transport of CH4 from the sediment; demethylation of organic compounds in oxic environments; photosynthesis, ebullition, and emission through macrophytes; and transport by various organisms. Nevertheless, the contribution of individual mechanisms to the accumulation and emission of methane is not well constrained. For example, the contribution of aerobic and anaerobic methane oxidizers to methane consumption in sediments and deeper layers of the water column at the oxic–anoxic interfaces is well studied. In contrast, in the oxic surface layers of oceans and lakes, this process is less understood with contradicting data regarding the inhibitory effects of light and oxygen on the methane oxidation process. As methane emissions are a result of production, transport, and consumption, it is essential to gain a better understanding of the organisms playing a role in the process as well as the different rates of production and consumption.
The variability in methane emissions from different types of aquatic systems and across various spatial scales, from ponds to large lakes, streams to rivers, estuaries, and oceans, hinders the generation of large-scale models. Novel methanogenesis processes discovered in the last decade are major contributors to methane emissions, yet there is minimal information on their isotopic signatures. Coupled, these two gaps in knowledge contribute to the large discrepancies between top-down and bottom-up approaches when evaluating the role of aquatic systems in the global methane budget.
We welcome contributions to this Special Issue addressing methane production, consumption, transport, and emissions from different aquatic bodies. Studies may relate to microbial communities involved in CH4 cycling, quantification of classic and novel processes and pathways, large-scale spatiotemporal studies, isotopic characterization of novel methane sources, as well as novel methodological approaches to quantify methane emissions from water.
All contributions to this Special Issue must fit within the scope of Limnology and Oceanography Letters (https://aslopubs.onlinelibrary.wiley.com/journal/23782242) and will be assessed with the same level of rigor as regular journal contributions. Accepted papers will be published online in Early View with a permanent DOI. A Virtual Issue of papers submitted to this Special Issue will be bound and added to the journal website collections page. All articles are Open Access, and the publication cost is US$ 2688 for ASLO members and $3360 for nonmembers. The membership cost is only $30 for students and emeritus scientists, $50 for Early Career Scientists, and no cost for students and Early Career Scientists from developing countries (see: https://www.aslo.org/membership-options-join-and-renew/join/). Waivers and discounts of article publication charges are available to corresponding authors based in low- and lower-middle income countries and locations (details: https://aslopubs.onlinelibrary.wiley.com/hub/journal/23782242/resources/apc#:~:text=The%20journal%20does%20not%20charge%20any%20submission%20fees%20or%20page%20charges). Please note the journal's data publication requirement as described in Cloern (2022).
To determine suitability of a manuscript to the special issue, please submit a 250–300 words manuscript proposal (presubmission inquiry) by 30 September 2024 to the Editor in Chief of Limnology and Oceanography Letters, James E. Cloern at: [email protected], who will forward the inquiries to the SI editors for evaluation. Manuscript submissions are expected by 30 June 2025.
期刊介绍:
All past issues of the Limnology and Oceanography Bulletin are available online, including its predecessors Communications to Members and the ASLO Bulletin. Access to the current and previous volume is restricted to members and institutions with a subscription to the ASLO journals. All other issues are freely accessible without a subscription. As part of ASLO’s mission to disseminate and communicate knowledge in the aquatic sciences.