COASTAL OCEAN ACIDIFICATION IN BRAZIL: A BRIEF OVERVIEW AND PERSPECTIVES

Luiz Carlos Cotovicz Jr., Rozane Valente Marins, G. Abril
{"title":"COASTAL OCEAN ACIDIFICATION IN BRAZIL: A BRIEF OVERVIEW AND PERSPECTIVES","authors":"Luiz Carlos Cotovicz Jr., Rozane Valente Marins, G. Abril","doi":"10.32360/acmar.v55iespecial.78514","DOIUrl":null,"url":null,"abstract":"This perspective paper aims at presenting the current knowledge on the processes of ocean acidification (OA) and coastal acidification (CA) in the Brazilian coastal ocean. We define and differentiate the processes of OA and CA: the first driven by the actual global increase of atmospheric carbon dioxide (CO2); the second driven by a combination of ocean uptake of atmospheric CO2 and other local/regional chemical additions or subtractions in aquatic ecosystems at the land-ocean interface. Regarding OA, we have centered our analysis on the data available for the main water masses along the Brazilian coast: South Atlantic Central Water (SACW), Tropical Water (TW), and Coastal Water (CW). The few data available for the shallow coastal waters (< 200 m depth) of the continental shelf reveal an increase in the anthropogenic component of the total dissolved inorganic carbon (DIC) pool in the SACW, with a decline in the ocean pH (over two decades; 1993-2013), and in the saturation state of calcium carbonate (CaCO3) minerals. We could not find OA trends for TW and CW because no data was available. Overall, the colder water masses (SACW, Plata Plume) have lower buffering capacity and simulations show that will potentially experience earlier negative OA impacts than the warmer waters masses (TW, Amazon Plume). Regarding CA, we have identified some local/regional studies investigating the carbonate chemistry in nearshore/estuarine ecosystems, particularly on the quantification of sources and sinks of CO2 , and determining short-term variabilities. Apparently, spreading coastal eutrophication in Brazil can enhances or reduces the process of OA, depending on the net ecosystem metabolism in combination with other chemical alterations. However, we could not find medium-long term acidification trends due to the limited data. There is a limited capacity to produce long time-series of carbonate chemistry parameters in key ecosystems and regions along the Brazilian coast. This lack of past information hinders and impairs the scientific community for identifying potential patterns of acidification along the Brazilian coast. We call for an urgent action in Brazil, with emphasis on the establishment of moored buoys/stations and/or scientific programs in the long term with continuous, real-time measurements of the main carbonate chemistry parameters. \nKeywords: ocean acidification, coastal acidification, coastal eutrophication, continental shelf, Southwestern Atlantic Ocean","PeriodicalId":410099,"journal":{"name":"Arquivos de Ciências do Mar","volume":"437 1","pages":"0"},"PeriodicalIF":0.0000,"publicationDate":"2022-03-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"1","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Arquivos de Ciências do Mar","FirstCategoryId":"1085","ListUrlMain":"https://doi.org/10.32360/acmar.v55iespecial.78514","RegionNum":0,"RegionCategory":null,"ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"","JCRName":"","Score":null,"Total":0}
引用次数: 1

Abstract

This perspective paper aims at presenting the current knowledge on the processes of ocean acidification (OA) and coastal acidification (CA) in the Brazilian coastal ocean. We define and differentiate the processes of OA and CA: the first driven by the actual global increase of atmospheric carbon dioxide (CO2); the second driven by a combination of ocean uptake of atmospheric CO2 and other local/regional chemical additions or subtractions in aquatic ecosystems at the land-ocean interface. Regarding OA, we have centered our analysis on the data available for the main water masses along the Brazilian coast: South Atlantic Central Water (SACW), Tropical Water (TW), and Coastal Water (CW). The few data available for the shallow coastal waters (< 200 m depth) of the continental shelf reveal an increase in the anthropogenic component of the total dissolved inorganic carbon (DIC) pool in the SACW, with a decline in the ocean pH (over two decades; 1993-2013), and in the saturation state of calcium carbonate (CaCO3) minerals. We could not find OA trends for TW and CW because no data was available. Overall, the colder water masses (SACW, Plata Plume) have lower buffering capacity and simulations show that will potentially experience earlier negative OA impacts than the warmer waters masses (TW, Amazon Plume). Regarding CA, we have identified some local/regional studies investigating the carbonate chemistry in nearshore/estuarine ecosystems, particularly on the quantification of sources and sinks of CO2 , and determining short-term variabilities. Apparently, spreading coastal eutrophication in Brazil can enhances or reduces the process of OA, depending on the net ecosystem metabolism in combination with other chemical alterations. However, we could not find medium-long term acidification trends due to the limited data. There is a limited capacity to produce long time-series of carbonate chemistry parameters in key ecosystems and regions along the Brazilian coast. This lack of past information hinders and impairs the scientific community for identifying potential patterns of acidification along the Brazilian coast. We call for an urgent action in Brazil, with emphasis on the establishment of moored buoys/stations and/or scientific programs in the long term with continuous, real-time measurements of the main carbonate chemistry parameters. Keywords: ocean acidification, coastal acidification, coastal eutrophication, continental shelf, Southwestern Atlantic Ocean
查看原文
分享 分享
微信好友 朋友圈 QQ好友 复制链接
本刊更多论文
巴西沿海海洋酸化:简要概述和展望
这篇观点论文旨在介绍目前巴西沿海海洋海洋酸化(OA)和海岸酸化(CA)过程的知识。我们定义并区分了OA和CA的过程:第一个过程是由全球大气二氧化碳(CO2)的实际增加驱动的;第二种是海洋对大气二氧化碳的吸收以及陆地-海洋界面水生生态系统中其他局部/区域化学物质的增减共同作用的结果。关于OA,我们集中分析了巴西沿海主要水团的可用数据:南大西洋中部水(SACW)、热带水(TW)和沿海水(CW)。大陆架浅海水域(< 200 m深度)的少量数据显示,SACW中总溶解无机碳(DIC)池的人为成分增加,海洋pH值(20年来)下降;1993-2013),并处于饱和状态的碳酸钙(CaCO3)矿物。由于没有数据,我们无法找到TW和CW的OA趋势。总的来说,较冷的水团(SACW, Plata羽流)具有较低的缓冲能力,模拟表明,与较温暖的水团(TW,亚马逊羽流)相比,可能会更早地经历负OA影响。在CA方面,我们已经确定了一些局部/区域研究,调查了近岸/河口生态系统中的碳酸盐化学,特别是对CO2源和汇的量化,并确定了短期变率。显然,巴西沿海富营养化的扩散可以增强或减少OA的过程,这取决于净生态系统代谢与其他化学变化的结合。然而,由于数据有限,我们无法找到中长期酸化趋势。在巴西沿海的关键生态系统和地区,生产碳酸盐化学参数的长时间序列的能力有限。过去信息的缺乏阻碍和损害了科学界确定巴西海岸酸化的潜在模式。我们呼吁在巴西采取紧急行动,重点是建立系泊浮标/站和/或科学计划,长期持续实时测量主要碳酸盐化学参数。关键词:海洋酸化,海岸酸化,海岸富营养化,大陆架,西南大西洋
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 去求助
来源期刊
自引率
0.00%
发文量
0
期刊最新文献
OCCURRENCE OF IMMATURE SHARKS IN ARTISANAL FISHERIES OF THE SOUTHERN GULF OF MEXICO BASELINE DATA ON RUBIDIUM (Rb) CONTAMINATION IN JUVENILE CARIBBEAN SHARPNOSE SHARK Rhizoprionodon porosus FROM SOUTHEASTERN BRAZI PRIMEIRO REGISTRO DOCUMENTADO DO CAMARÃO-TIGRE-GIGANTE, Penaeus monodon (Fabricius, 1798), NO LITORAL DO CEARÁ, NORDESTE DO BRASIL MOLECULAR IDENTIFICATION OF SHARK MEAT TRADED AS CAÇÃO IN SOUTHWESTERN STATE OF SÃO PAULO, BRAZIL PERFIL NUTRICIONAL DO POLIQUETA Laeonereis acuta (Treadwell, 1923): ALTERNATIVA DE ALIMENTO PARA AQUICULTURA
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
现在去查看 取消
×
提示
确定
0
微信
客服QQ
Book学术公众号 扫码关注我们
反馈
×
意见反馈
请填写您的意见或建议
请填写您的手机或邮箱
已复制链接
已复制链接
快去分享给好友吧!
我知道了
×
扫码分享
扫码分享
Book学术官方微信
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术
文献互助 智能选刊 最新文献 互助须知 联系我们:info@booksci.cn
Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。
Copyright © 2023 Book学术 All rights reserved.
ghs 京公网安备 11010802042870号 京ICP备2023020795号-1