In 2019,an oil spill in Brazil,of unknown origin,severely impacted coastal environs with the worst environmental disaster ever recorded in any tropical coastal region globally severely damaging South Pirangi Reef area...In 2019,an oil spill in Brazil,of unknown origin,severely impacted coastal environs with the worst environmental disaster ever recorded in any tropical coastal region globally severely damaging South Pirangi Reef area in the state of Rio Grande do Norte(RN).Here we discuss acute and chronic impacts including chemical contamination and economic consequences all over the world and show some evidence of the oil spill in this biodiverse area.Moreover,the lapse between the moment of the disastei;and the action to manage it,was hampered by a political agenda coinciding with local and global tragedies that redirected public attention.Meanwhile almost 2 years have passed still without the offending party identification or culpability;and poor communities may continue to absorb its deleterious impacts for decades without consideration or compensation.This disaster occurred during the Brazilian government's current issues involving extensive environmental mismanagement,resulting in a slow response from an inept system.It is with urgent necessity to spotlight this tragedy in this unique and sensitive reef habitat experiencing the ongoing damaging effects that include socio-economic losses not yet addressed.展开更多
We use the excellent sediment recovery of International Ocean Discovery Program(IODP)Exp.363,in the Western Pacific Warm Pool(WPWP)to assess down-core variations in the abundance of warm versus cool benthic foraminife...We use the excellent sediment recovery of International Ocean Discovery Program(IODP)Exp.363,in the Western Pacific Warm Pool(WPWP)to assess down-core variations in the abundance of warm versus cool benthic foraminiferal species through a warm benthic foraminifers(WBF)curve.The total percentage of the“warm”shallower species group(Laticarinina pauperata,Cibicidoides kullenbergi,C.robertsonianus,Cibicidoides sp.,Hoeglundina elegans,and Bulimina aculeata)and of the“cool”species group from deep waters(Pyrgo murrhina,Planulina wuellerstorfi,Uvigerina peregrina,and Globobulimina hoeglundi,Hopkinsina pacifica)at all sites is used to assess paleo temporal and spatial variations in preservation and marine temperature.Our study sites span water depths ranging from 875 m to 3421 m and our results indicate that well-preserved living and fossil foraminifera characterize mudline and core sediments at all water depths attesting the wide environmental tolerance of these species to temperature and pressure.Using magneto-and biostratigraphy datum,these sediments are of Oligocene age.Our low-resolution study showed that with the exception of core 1486B which the linear tendency of warmer species is toward cool sediments in old times,all of them show that older sediments indicate warmer periods than today,which is expected from Miocene to Recent.Our results provide evidence for the preservation potential of deeply buried sediments,which has implications on climate reconstructions based on the population dynamics of calcareous benthic foraminifera.展开更多
The environmental quality of the marine area close to the Landulpho Alves Oil Refinery situated in Todosos Santos Bay (Bahia, Brazil) was assessed by statistical methods on foraminiferal assemblages, with species tole...The environmental quality of the marine area close to the Landulpho Alves Oil Refinery situated in Todosos Santos Bay (Bahia, Brazil) was assessed by statistical methods on foraminiferal assemblages, with species tolerant to low continental influence such as Ammonia tepida, Elphidium excavatum, Pseudononion atlanticum and Quinqueloculina spp., and to high organic matter such as Buliminella elegantissima and Bulimina marginata. We have found that Bolivina pulchella, Pseudononion atlanticum, Fursenkoina pontoni, Buliminella elegantissima, Bolivina striatula, Bulimina marginata, Quinqueloculina spp., Ammonia tepida, and Elphidium excavatum are opportunistic and tolerant to high levels of accumulated organic matter, and are associated to stations 6, 17, 18, 19, 21, 22, 23, 24, and 25, located mainly in the southern, outermost part of the Bay.展开更多
We aim to evaluate the quality of the Guanabara Bay sediments and the ecological changes due to the PETROBRAS crude oil leak in January 2000. Twenty-six sediment samples collected in July 2000 and in February 2001 wer...We aim to evaluate the quality of the Guanabara Bay sediments and the ecological changes due to the PETROBRAS crude oil leak in January 2000. Twenty-six sediment samples collected in July 2000 and in February 2001 were analyzed for pH, dissolved oxygen, and foraminiferal composition. In the northwest and central parts of the bay, low oxygen dissolved values are related to waste discharges with the dominance of Buliminella elegantissima. In winter, near Iguaçu River, the pH of the sediment is low, therefore highly acidic. The acidity is responsible for the foraminiferal low diversity limiting the occurrence of species with fragile tests. On the other hand, thicker tests of Elphidium spp. disappeared last, therefore increasing its relative dominance in winter. In summer, this is a barren zone. The explanation lies in the continuous dissolution of tests that culminated with the total disappearance of these microorganisms one year after the accident.展开更多
基金This work was carried out under the scope of INCT AmbTropic phase II(CNPq Process 465634/2014-1)linked to the Emergency Action to combat the 2019 oil spill of the MCTI(DTI-A 381360/2020-2 fellowship to PPB Eichler)We are grateful to the ANP-PRH 22 and the CAPES(Coordenacao de Aperfeipoamento de Pessoal de Nivel Superior)Project"Oceanographic process in the breaking of the continental shelf of northeastern Brazil:Scientific foundations for special marine planning"for the finan cial assistance granted,to the crews of the vessels used,and to all colleagues of GGEMMAAJFRNWe are grateful to CAPES(Coordenavao de Aperfeipoamento de Pessoal de Nivel Superior)for funding support through Projects Special Visiting Professor(PVE 151-2012,Aux Pe 242-2013),and Ciencias do Mar II(23038.004320/2014-1)that enabled a Pos Doc fellowship for P.P.B.Eichler at Moss Landing Marine Laboratories of San Jose State University(MLML/SJSU),and at the Ocean Sciences Department of the University of California at Santa Cruz(UCSC)(88887.305531/2018-00,88881.188496/2018-01 and 9999.000098/2017-05).We are also thankful to CNPq for the research grants for co-author Gomes M.P(PQ 302483/2019-5)and for co-author Vital H(PQ 311413/2016-1,PQ 315742/2020-8),and to OSC Oceanica for supporting Liana Mendes throughout the research.
文摘In 2019,an oil spill in Brazil,of unknown origin,severely impacted coastal environs with the worst environmental disaster ever recorded in any tropical coastal region globally severely damaging South Pirangi Reef area in the state of Rio Grande do Norte(RN).Here we discuss acute and chronic impacts including chemical contamination and economic consequences all over the world and show some evidence of the oil spill in this biodiverse area.Moreover,the lapse between the moment of the disastei;and the action to manage it,was hampered by a political agenda coinciding with local and global tragedies that redirected public attention.Meanwhile almost 2 years have passed still without the offending party identification or culpability;and poor communities may continue to absorb its deleterious impacts for decades without consideration or compensation.This disaster occurred during the Brazilian government's current issues involving extensive environmental mismanagement,resulting in a slow response from an inept system.It is with urgent necessity to spotlight this tragedy in this unique and sensitive reef habitat experiencing the ongoing damaging effects that include socio-economic losses not yet addressed.
基金We are thankful for the Project Geohazards and Tectonics(CAPES Grant 88887.091714/2014-01,IODP Program)Research was also supported by IODP/CAPES Brazil fellowship granted to PE to go aboard the Research Vessel Joides Resolution in 2016.This research would not have been conduct without funding from Ciências do Mar II(CAPES Coordenação de Aperfeiçoamento de Pessoal de Nível Superior)through the Project Processos oceanográficos na quebra da plataforma continental do nordeste brasileiro:fundamentos científicos para o planejamento espacial marinho(n°43/2013,23038.004320/2014-11)through for the Post-Doc Fellowship for Eichler at the Moss Landing Marine Laboratories of the San Jose State University(MLML/SJSU)+1 种基金at the Ocean Sciences Department of the University of California at Santa Cruz(UCSC)(grants Nº88887.305531/2018-00,Nº88881.188496/2018-01)We are also grateful for the International Ocean Discovery Program(IODP)in the Texas A&M University(USA)(Grant Nº9999.000098/2017-05)and to the Technical Support to Strengthen National Palaeontology(Apoio Técnico para Fortalecimento da Paleontologia Nacional,Ministério da Ciência e Tecnologia MCTI/National Research Council CNPq Nº23/2011,Nº552976/2011-3)for funding opportunity.We are grateful for the EcoLogicProject for the manuscript detailed editing.
文摘We use the excellent sediment recovery of International Ocean Discovery Program(IODP)Exp.363,in the Western Pacific Warm Pool(WPWP)to assess down-core variations in the abundance of warm versus cool benthic foraminiferal species through a warm benthic foraminifers(WBF)curve.The total percentage of the“warm”shallower species group(Laticarinina pauperata,Cibicidoides kullenbergi,C.robertsonianus,Cibicidoides sp.,Hoeglundina elegans,and Bulimina aculeata)and of the“cool”species group from deep waters(Pyrgo murrhina,Planulina wuellerstorfi,Uvigerina peregrina,and Globobulimina hoeglundi,Hopkinsina pacifica)at all sites is used to assess paleo temporal and spatial variations in preservation and marine temperature.Our study sites span water depths ranging from 875 m to 3421 m and our results indicate that well-preserved living and fossil foraminifera characterize mudline and core sediments at all water depths attesting the wide environmental tolerance of these species to temperature and pressure.Using magneto-and biostratigraphy datum,these sediments are of Oligocene age.Our low-resolution study showed that with the exception of core 1486B which the linear tendency of warmer species is toward cool sediments in old times,all of them show that older sediments indicate warmer periods than today,which is expected from Miocene to Recent.Our results provide evidence for the preservation potential of deeply buried sediments,which has implications on climate reconstructions based on the population dynamics of calcareous benthic foraminifera.
文摘The environmental quality of the marine area close to the Landulpho Alves Oil Refinery situated in Todosos Santos Bay (Bahia, Brazil) was assessed by statistical methods on foraminiferal assemblages, with species tolerant to low continental influence such as Ammonia tepida, Elphidium excavatum, Pseudononion atlanticum and Quinqueloculina spp., and to high organic matter such as Buliminella elegantissima and Bulimina marginata. We have found that Bolivina pulchella, Pseudononion atlanticum, Fursenkoina pontoni, Buliminella elegantissima, Bolivina striatula, Bulimina marginata, Quinqueloculina spp., Ammonia tepida, and Elphidium excavatum are opportunistic and tolerant to high levels of accumulated organic matter, and are associated to stations 6, 17, 18, 19, 21, 22, 23, 24, and 25, located mainly in the southern, outermost part of the Bay.
文摘We aim to evaluate the quality of the Guanabara Bay sediments and the ecological changes due to the PETROBRAS crude oil leak in January 2000. Twenty-six sediment samples collected in July 2000 and in February 2001 were analyzed for pH, dissolved oxygen, and foraminiferal composition. In the northwest and central parts of the bay, low oxygen dissolved values are related to waste discharges with the dominance of Buliminella elegantissima. In winter, near Iguaçu River, the pH of the sediment is low, therefore highly acidic. The acidity is responsible for the foraminiferal low diversity limiting the occurrence of species with fragile tests. On the other hand, thicker tests of Elphidium spp. disappeared last, therefore increasing its relative dominance in winter. In summer, this is a barren zone. The explanation lies in the continuous dissolution of tests that culminated with the total disappearance of these microorganisms one year after the accident.