Stacey L Felgate, John Aldridge, Stefan G Bolam, Sarah Breimann, Emil de Borger, Jolien Claes, Jochen Depestele, Graham Epstein, Clement Garcia, Natalie Hicks, Michel Kaiser, Jack H Laverick, Gennadi Lessin, Finbarr G O'Neill, Sarah Paradis, Ruth Parker, Ryan Pereira, Alex J Poulton, Claire Powell, Craig Smeaton, Paul Snelgrove, Justin Tiano, Johan van der Molen, Sebastiaan van de Velde, Marija Sciberras
{"title":"调查移动式底层捕捞对底栖生物碳处理和储存的影响:系统综述协议。","authors":"Stacey L Felgate, John Aldridge, Stefan G Bolam, Sarah Breimann, Emil de Borger, Jolien Claes, Jochen Depestele, Graham Epstein, Clement Garcia, Natalie Hicks, Michel Kaiser, Jack H Laverick, Gennadi Lessin, Finbarr G O'Neill, Sarah Paradis, Ruth Parker, Ryan Pereira, Alex J Poulton, Claire Powell, Craig Smeaton, Paul Snelgrove, Justin Tiano, Johan van der Molen, Sebastiaan van de Velde, Marija Sciberras","doi":"10.1186/s13750-024-00348-z","DOIUrl":null,"url":null,"abstract":"<p><strong>Background: </strong>Marine sediments represent one of the planet's largest carbon stores. Bottom trawl fisheries constitute the most widespread physical disturbance to seabed habitats, which exert a large influence over the oceanic carbon dioxide (CO<sub>2</sub>) sink. 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引用次数: 0
摘要
背景:海洋沉积物是地球上最大的碳储存库之一。底拖网渔业是对海底生境最广泛的物理干扰,而海底生境对海洋二氧化碳(CO2)汇有很大影响。最近的研究引发了人们的关注,即拖网捕捞对海床的扰动会因此将海洋沉积物变成一个巨大的二氧化碳源,但其中涉及的计算具有很大的不确定性。这主要是由于对拖网如何混合和重新悬浮沉积物,如何改变生物扰动、生物灌溉和充氧率,以及这些过程如何转化为进入或流出沉积物的碳通量缺乏定量了解:方法:本综述规程探讨的主要问题是:移动底层捕捞如何影响底栖生物的碳处理和储存?这一问题将分为以下次要问题:移动底层捕捞对以下方面有何影响:(i) 底栖沉积物中碳的数量和类型;(ii) 底栖-远洋碳通量的大小和方向;(iii) 控制底栖碳归宿的生物地球化学、生物和物理参数;(iv) 控制再悬浮碳归宿的生物地球化学、生物和物理参数。将在 Web of Science、SCOPUS、PROQUEST 以及一系列灰色和专业资料来源中进行文献检索。科学网的初步范围检索为最终的检索字符串提供了依据,该字符串是根据人口干预比较结果(PICO)原则制定的。符合条件的研究必须包含有关移动底层捕捞导致相关人群变化的数据。符合条件的研究设计包括前后研究、控制和影响研究以及梯度研究。将对全文筛选出的研究进行严格评估,并提取研究结果。提取的数据将存储在 Excel 电子表格中。将使用包括森林图在内的各种可视化工具对结果进行叙述性和定量综合报告。在数据充足的情况下,将进行元分析。
Investigating the effects of mobile bottom fishing on benthic carbon processing and storage: a systematic review protocol.
Background: Marine sediments represent one of the planet's largest carbon stores. Bottom trawl fisheries constitute the most widespread physical disturbance to seabed habitats, which exert a large influence over the oceanic carbon dioxide (CO2) sink. Recent research has sparked concern that seabed disturbance from trawling can therefore turn marine sediments into a large source of CO2, but the calculations involved carry a high degree of uncertainty. This is primarily due to a lack of quantitative understanding of how trawling mixes and resuspends sediments, how it alters bioturbation, bioirrigation, and oxygenation rates, and how these processes translate into carbon fluxes into or out of sediments.
Methods: The primary question addressed by this review protocol is: how does mobile bottom fishing affect benthic carbon processing and storage? This question will be split into the following secondary questions: what is the effect of mobile bottom fishing on: (i) the amount and type of carbon found in benthic sediments; (ii) the magnitude and direction of benthic-pelagic carbon fluxes; (iii) the biogeochemical, biological, and physical parameters that control the fate of benthic carbon; and (iv) the biogeochemical, biological, and physical parameters that control the fate of resuspended carbon. Literature searches will be conducted in Web of Science, SCOPUS, PROQUEST, and a range of grey and specialist sources. An initial scoping search in Web of Science informed the final search string, which has been formulated according to Population Intervention Comparator Outcome (PICO) principles. Eligible studies must contain data concerning a change in a population of interest caused by mobile bottom fishing. Eligible study designs are Before and After, Control and Impact, and Gradient studies. Studies included at full-text screening will be critically appraised, and study findings will be extracted.Extracted data will be stored in an Excel spreadsheet. Results will be reported in narrative and quantitative syntheses using a variety of visual tools including forest plots. Meta-analysis will be conducted where sufficient data exists.