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Herndl GJ, Bayer B, Baltar F, Reinthaler T. Prokaryotic Life in the Deep Ocean's Water Column. ANNUAL REVIEW OF MARINE SCIENCE 2023; 15:461-483. [PMID: 35834811 DOI: 10.1146/annurev-marine-032122-115655] [Citation(s) in RCA: 9] [Impact Index Per Article: 9.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 06/15/2023]
Abstract
The oceanic waters below a depth of 200 m represent, in terms of volume, the largest habitat of the biosphere, harboring approximately 70% of the prokaryotic biomass in the oceanic water column. These waters are characterized by low temperature, increasing hydrostatic pressure, and decreasing organic matter supply with depth. Recent methodological advances in microbial oceanography have refined our view of the ecology of prokaryotes in the dark ocean. Here, we review the ecology of prokaryotes of the dark ocean, present data on the biomass distribution and heterotrophic and chemolithoautotrophic prokaryotic production in the major oceanic basins, and highlight the phylogenetic and functional diversity of this part of the ocean. We describe the connectivity of surface and deep-water prokaryotes and the molecular adaptations of piezophilic prokaryotes to high hydrostatic pressure. We also highlight knowledge gaps in the ecology of the dark ocean's prokaryotes and their role in the biogeochemical cycles in the largest habitat of the biosphere.
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Affiliation(s)
- Gerhard J Herndl
- Department of Functional and Evolutionary Ecology, University of Vienna, Vienna, Austria;
- Department of Marine Microbiology and Biogeochemistry, Royal Netherlands Institute for Sea Research (NIOZ), Utrecht University, Den Burg, The Netherlands
| | - Barbara Bayer
- Department of Microbiology and Ecosystem Science, Centre for Microbiology and Environmental Systems Science, University of Vienna, Vienna, Austria
| | - Federico Baltar
- Department of Functional and Evolutionary Ecology, University of Vienna, Vienna, Austria;
| | - Thomas Reinthaler
- Department of Functional and Evolutionary Ecology, University of Vienna, Vienna, Austria;
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2
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Orta-Ponce CP, Rodríguez-Ramos T, Nieto-Cid M, Teira E, Guerrero-Feijóo E, Bode A, Varela MM. Empirical leucine-to-carbon conversion factors in north-eastern Atlantic waters (50-2000 m) shaped by bacterial community composition and optical signature of DOM. Sci Rep 2021; 11:24370. [PMID: 34934099 PMCID: PMC8692456 DOI: 10.1038/s41598-021-03790-y] [Citation(s) in RCA: 1] [Impact Index Per Article: 0.3] [Reference Citation Analysis] [Abstract] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 07/23/2021] [Accepted: 11/09/2021] [Indexed: 11/09/2022] Open
Abstract
Microbial heterotrophic activity is a major process regulating the flux of dissolved organic matter (DOM) in the ocean, while the characteristics of this DOM strongly influence its microbial utilization and fate in the ocean. In order to broaden the vertical resolution of leucine-to-carbon conversion factors (CFs), needed for converting substrate incorporation into biomass production by heterotrophic bacteria, 20 dilution experiments were performed in the North Atlantic Ocean. We found a depth-stratification in empirical CFs values from epipelagic to bathypelagic waters (4.00 ± 1.09 to 0.10 ± 0.00 kg C mol Leu−1). Our results demonstrated that the customarily used theoretical CF of 1.55 kg C mol Leu−1 in oceanic samples can lead to an underestimation of prokaryotic heterotrophic production in epi- and mesopelagic waters, while it can overestimate it in the bathypelagic ocean. Pearson correlations showed that CFs were related not only to hydrographic variables such as temperature, but also to specific phylogenetic groups and DOM quality and quantity indices. Furthermore, a multiple linear regression model predicting CFs from relatively simple hydrographic and optical spectroscopic measurements was attempted. Taken together, our results suggest that differences in CFs throughout the water column are significantly connected to DOM, and also reflect differences linked to specific prokaryotic groups.
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Affiliation(s)
- C Pamela Orta-Ponce
- Instituto Español de Oceanografía (IEO-CSIC), Centro Oceanográfico de A Coruña, 15080, A Coruña, Spain. .,Facultade de Ciencias, Zapateira, Universidade da Coruña, 15071, A Coruña, Spain.
| | - Tamara Rodríguez-Ramos
- Instituto Español de Oceanografía (IEO-CSIC), Centro Oceanográfico de A Coruña, 15080, A Coruña, Spain
| | - Mar Nieto-Cid
- Instituto Español de Oceanografía (IEO-CSIC), Centro Oceanográfico de A Coruña, 15080, A Coruña, Spain.,Laboratorio de Geoquímica Orgánica, Instituto de Investigaciones Marinas (CSIC), 36208, Vigo, Spain
| | - Eva Teira
- Departamento de Ecología y Biología Animal, Universidade de Vigo, Centro de Investigación Mariña da Universidade de Vigo (CIM-UVigo), 36310, Vigo, Spain
| | - Elisa Guerrero-Feijóo
- Instituto Español de Oceanografía (IEO-CSIC), Centro Oceanográfico de A Coruña, 15080, A Coruña, Spain
| | - Antonio Bode
- Instituto Español de Oceanografía (IEO-CSIC), Centro Oceanográfico de A Coruña, 15080, A Coruña, Spain
| | - Marta M Varela
- Instituto Español de Oceanografía (IEO-CSIC), Centro Oceanográfico de A Coruña, 15080, A Coruña, Spain
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González-Gaya B, Casal P, Jurado E, Dachs J, Jiménez B. Vertical transport and sinks of perfluoroalkyl substances in the global open ocean. ENVIRONMENTAL SCIENCE. PROCESSES & IMPACTS 2019; 21:1957-1969. [PMID: 31393489 DOI: 10.1039/c9em00266a] [Citation(s) in RCA: 19] [Impact Index Per Article: 3.8] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Indexed: 05/20/2023]
Abstract
The ubiquitous occurrence of perfluoroalkyl substances (PFAS) in the open ocean has been previously documented, but their vertical transport and oceanic sinks have not been comprehensively characterized and quantified at the oceanic scale. During the Malaspina 2010 circumnavigation expedition, 21 PFAS were measured at the surface and at the deep chlorophyll maximum (DCM) in the Atlantic, Indian and Pacific oceans. In this work, we report an extended data set of PFAS dissolved phase concentrations at the DCM. ∑PFAS at the DCM varied from 130 to 11 000 pg L-1, with a global average value of 500 pg L-1. Perfluorooctanesulfonate (PFOS) abundance contributed 39% of ∑PFAS, followed by perfluorodecanoate (PFDA, 17%), and perfluorohexanoate (PFHxA, 12%). The relative contribution of the remaining compounds was below 10%, with perfluorooctanoate (PFOA) contributing only 5% to PFAS measured at the DCM. Estimates of vertical diffusivity, derived from microstructure turbulence observations in the upper (<300 m) water column, allowed the derivation of PFAS eddy diffusive fluxes from concurrent field measurements of eddy diffusivity and PFAS concentrations. The PFAS concentrations at the DCM predicted from an eddy diffusivity model were lower than field-measured concentrations, suggesting a relevant role of other vertical transport mechanisms. Settling fluxes of organic matter bound PFAS (biological pump), oceanic circulation and potential, yet un-reported, biological transformations are discussed.
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Affiliation(s)
- Belén González-Gaya
- Department of Instrumental Analysis and Environmental Chemistry, Institute of Organic Chemistry (IQOG-CSIC), Juan de la Cierva 3, 28006 Madrid, Spain. and Department of Environmental Chemistry, Institute of Environmental Assessment and Water Research, Spanish National Research Council (IDAEA-CSIC), Jordi Girona 18-26, 08034 Barcelona, Catalonia, Spain and Department of Analytical Chemistry, Plentzia Marine Station of the University of the Basque Country (EHU/UPV), Areatza Pasealekua 47, 48620 Plentzia, Basque Country, Spain
| | - Paulo Casal
- Department of Environmental Chemistry, Institute of Environmental Assessment and Water Research, Spanish National Research Council (IDAEA-CSIC), Jordi Girona 18-26, 08034 Barcelona, Catalonia, Spain
| | - Elena Jurado
- Department of Environmental Chemistry, Institute of Environmental Assessment and Water Research, Spanish National Research Council (IDAEA-CSIC), Jordi Girona 18-26, 08034 Barcelona, Catalonia, Spain and Engineering Department, La Salle Campus Barcelona, Ramon Llull University (URL), Sant Joan de la Salle, 42, 08022 Barcelona, Catalonia, Spain
| | - Jordi Dachs
- Department of Environmental Chemistry, Institute of Environmental Assessment and Water Research, Spanish National Research Council (IDAEA-CSIC), Jordi Girona 18-26, 08034 Barcelona, Catalonia, Spain
| | - Begoña Jiménez
- Department of Instrumental Analysis and Environmental Chemistry, Institute of Organic Chemistry (IQOG-CSIC), Juan de la Cierva 3, 28006 Madrid, Spain.
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4
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Sisma-Ventura G, Rahav E. DOP Stimulates Heterotrophic Bacterial Production in the Oligotrophic Southeastern Mediterranean Coastal Waters. Front Microbiol 2019; 10:1913. [PMID: 31474972 PMCID: PMC6706821 DOI: 10.3389/fmicb.2019.01913] [Citation(s) in RCA: 16] [Impact Index Per Article: 3.2] [Reference Citation Analysis] [Abstract] [Key Words] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 04/24/2019] [Accepted: 08/05/2019] [Indexed: 11/13/2022] Open
Abstract
Phytoplankton and heterotrophic bacteria rely on a suite of inorganic and organic macronutrients to satisfy their cellular needs. Here, we explored the effect of dissolved inorganic phosphate (PO4) and several dissolved organic molecules containing phosphorus [ATP, glucose-6-phosphate, 2-aminoethylphosphonic acid, collectively referred to as dissolved organic phosphorus (DOP)], on the activity and biomass of autotrophic and heterotrophic microbial populations in the coastal water of the southeastern Mediterranean Sea (SEMS) during summertime. To this end, surface waters were supplemented with PO4, one of the different organic molecules, or PO4 + ATP, and measured the PO4 turnover time (Tt), alkaline phosphatase activity (APA), heterotrophic bacterial production (BP), primary production (PP), and the abundance of the different microbial components. Our results show that PO4 alone does not stimulate any significant change in most of the autotrophic or heterotrophic bacterial variables tested. ATP addition (alone or with PO4) triggers the strongest increase in primary and bacterial productivity or biomass. Heterotrophic bacterial abundance and BP respond faster than phytoplankton (24 h post addition) to the various additions of DOP or PO4 + ATP, followed by a recovery of primary productivity (48 h post addition). These observations suggest that both autotrophic and heterotrophic microbial communities compete for labile organic molecules containing P, such as ATP, to satisfy their cellular needs. It also suggests that SEMS coastal water heterotrophic bacteria are likely C and P co-limited.
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Affiliation(s)
- Guy Sisma-Ventura
- Israel Oceanographic and Limnological Research, National Institute of Oceanography, Haifa, Israel
| | - Eyal Rahav
- Israel Oceanographic and Limnological Research, National Institute of Oceanography, Haifa, Israel
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Clifford EL, Varela MM, De Corte D, Bode A, Ortiz V, Herndl GJ, Sintes E. Taurine Is a Major Carbon and Energy Source for Marine Prokaryotes in the North Atlantic Ocean off the Iberian Peninsula. MICROBIAL ECOLOGY 2019; 78:299-312. [PMID: 30666368 PMCID: PMC6647121 DOI: 10.1007/s00248-019-01320-y] [Citation(s) in RCA: 25] [Impact Index Per Article: 5.0] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 06/28/2018] [Accepted: 01/03/2019] [Indexed: 05/31/2023]
Abstract
Taurine, an amino acid-like compound, acts as an osmostress protectant in many marine metazoans and algae and is released via various processes into the oceanic dissolved organic matter pool. Taurine transporters are widespread among members of the marine prokaryotic community, tentatively indicating that taurine might be an important substrate for prokaryotes in the ocean. In this study, we determined prokaryotic taurine assimilation and respiration throughout the water column along two transects in the North Atlantic off the Iberian Peninsula. Taurine assimilation efficiency decreased from the epipelagic waters from 55 ± 14% to 27 ± 20% in the bathypelagic layers (means of both transects). Members of the ubiquitous alphaproteobacterial SAR11 clade accounted for a large fraction of cells taking up taurine, especially in surface waters. Archaea (Thaumarchaeota + Euryarchaeota) were also able to take up taurine in the upper water column, but to a lower extent than Bacteria. The contribution of taurine assimilation to the heterotrophic prokaryotic carbon biomass production ranged from 21% in the epipelagic layer to 16% in the bathypelagic layer. Hence, we conclude that dissolved free taurine is a significant carbon and energy source for prokaryotes throughout the oceanic water column being utilized with similar efficiencies as dissolved free amino acids.
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Affiliation(s)
- Elisabeth L Clifford
- Department of Limnology and Bio-Oceanography, Center of Functional Ecology, University of Vienna, Althanstrasse 14, 1090, Vienna, Austria
| | - Marta M Varela
- Instituto Español de Oceanografía (IEO), Centro Oceanográfico de A Coruña, Apdo 130, 15080, A Coruña, Spain
| | - Daniele De Corte
- Research and Development Center for Marine Biosciences, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Natushima 2-15, Yokosuka, Kanagawa, 237-0061, Japan
| | - Antonio Bode
- Instituto Español de Oceanografía (IEO), Centro Oceanográfico de A Coruña, Apdo 130, 15080, A Coruña, Spain
| | - Victor Ortiz
- Department of Limnology and Bio-Oceanography, Center of Functional Ecology, University of Vienna, Althanstrasse 14, 1090, Vienna, Austria
| | - Gerhard J Herndl
- Department of Limnology and Bio-Oceanography, Center of Functional Ecology, University of Vienna, Althanstrasse 14, 1090, Vienna, Austria
- Royal Netherlands Institute for Sea Research (NIOZ), Department of Marine Microbiology and Biogeochemistry, Utrecht University, PO Box 59, 1790 AB, Den Burg, The Netherlands
| | - Eva Sintes
- Department of Limnology and Bio-Oceanography, Center of Functional Ecology, University of Vienna, Althanstrasse 14, 1090, Vienna, Austria.
- Instituto Español de Oceanografía (IEO), Centro Oceanográfico de Baleares, Moll de Ponent s/n, 07015, Palma de Mallorca, Spain.
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6
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Teira E, Logares R, Gutiérrez‐Barral A, Ferrera I, Varela MM, Morán XAG, Gasol JM. Impact of grazing, resource availability and light on prokaryotic growth and diversity in the oligotrophic surface global ocean. Environ Microbiol 2019; 21:1482-1496. [DOI: 10.1111/1462-2920.14581] [Citation(s) in RCA: 17] [Impact Index Per Article: 3.4] [Reference Citation Analysis] [Track Full Text] [Journal Information] [Subscribe] [Scholar Register] [Received: 03/23/2018] [Revised: 02/26/2019] [Accepted: 03/02/2019] [Indexed: 12/14/2022]
Affiliation(s)
- Eva Teira
- Departamento de Ecoloxía e Bioloxía AnimalUniversidade de Vigo Vigo Spain
| | - Ramiro Logares
- Departamento de Biologia Marina i OceanografiaInstitut de Ciències del Mar, CSIC Barcelona Catalonia Spain
| | | | - Isabel Ferrera
- Departamento de Biologia Marina i OceanografiaInstitut de Ciències del Mar, CSIC Barcelona Catalonia Spain
- Instituto Español de OceanografíaCentro Oceanográfico de Málaga Fuengirola Spain
| | - Marta M. Varela
- Instituto Español de OceanografíaCentro Oceanográfico de A Coruña A Coruña Spain
| | - Xosé Anxelu G. Morán
- Red Sea Research Center, Division of Biological and Environmental Sciences and EngineeringKing Abdullah University of Science and Technology Thuwal Saudi Arabia
| | - Josep M. Gasol
- Departamento de Biologia Marina i OceanografiaInstitut de Ciències del Mar, CSIC Barcelona Catalonia Spain
- Centre for Marine Ecosystems ResearchEdith Cowan University Joondalup Western Australia Australia
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7
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Lara E, Vaqué D, Sà EL, Boras JA, Gomes A, Borrull E, Díez-Vives C, Teira E, Pernice MC, Garcia FC, Forn I, Castillo YM, Peiró A, Salazar G, Morán XAG, Massana R, Catalá TS, Luna GM, Agustí S, Estrada M, Gasol JM, Duarte CM. Unveiling the role and life strategies of viruses from the surface to the dark ocean. SCIENCE ADVANCES 2017; 3:e1602565. [PMID: 28913418 PMCID: PMC5587022 DOI: 10.1126/sciadv.1602565] [Citation(s) in RCA: 63] [Impact Index Per Article: 9.0] [Reference Citation Analysis] [Abstract] [MESH Headings] [Grants] [Track Full Text] [Subscribe] [Scholar Register] [Received: 10/24/2016] [Accepted: 08/09/2017] [Indexed: 05/31/2023]
Abstract
Viruses are a key component of marine ecosystems, but the assessment of their global role in regulating microbial communities and the flux of carbon is precluded by a paucity of data, particularly in the deep ocean. We assessed patterns in viral abundance and production and the role of viral lysis as a driver of prokaryote mortality, from surface to bathypelagic layers, across the tropical and subtropical oceans. Viral abundance showed significant differences between oceans in the epipelagic and mesopelagic, but not in the bathypelagic, and decreased with depth, with an average power-law scaling exponent of -1.03 km-1 from an average of 7.76 × 106 viruses ml-1 in the epipelagic to 0.62 × 106 viruses ml-1 in the bathypelagic layer with an average integrated (0 to 4000 m) viral stock of about 0.004 to 0.044 g C m-2, half of which is found below 775 m. Lysogenic viral production was higher than lytic viral production in surface waters, whereas the opposite was found in the bathypelagic, where prokaryotic mortality due to viruses was estimated to be 60 times higher than grazing. Free viruses had turnover times of 0.1 days in the bathypelagic, revealing that viruses in the bathypelagic are highly dynamic. On the basis of the rates of lysed prokaryotic cells, we estimated that viruses release 145 Gt C year-1 in the global tropical and subtropical oceans. The active viral processes reported here demonstrate the importance of viruses in the production of dissolved organic carbon in the dark ocean, a major pathway in carbon cycling.
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Affiliation(s)
- Elena Lara
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
- Institute of Marine Sciences, National Research Council (CNR-ISMAR), Castello 2737/F Arsenale-Tesa 104, 30122 Venezia, Italy
| | - Dolors Vaqué
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Elisabet Laia Sà
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Julia A. Boras
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Ana Gomes
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Encarna Borrull
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Cristina Díez-Vives
- School of Biotechnology and Biomolecular Sciences, Centre for Marine Bio-Innovation, University of New South Wales, Sydney, New South Wales 2052, Australia
| | - Eva Teira
- Departamento de Ecología y Biología Animal, Universidad de Vigo, University of Vigo, 36310 Vigo, Spain
| | - Massimo C. Pernice
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Francisca C. Garcia
- Centro Oceanográfico de Gijón/Xixón, Instituto Español de Oceanografía, Avenida Príncipe de Asturias, 70, 33212 Gijón/Xixón, Spain
| | - Irene Forn
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Yaiza M. Castillo
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Aida Peiró
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Guillem Salazar
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Xosé Anxelu G. Morán
- Red Sea Research Center, Division of Biological and Environmental Sciences and Engineering, King Abdullah University of Science and Technology, Thuwal 23955-6900, Saudi Arabia
| | - Ramon Massana
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Teresa S. Catalá
- Instituto de Investigaciones Marinas, CSIC, Eduardo Cabello, 6, 36208 Vigo, Spain
- Departamento de Ecología and Instituto del Agua, Universidad de Granada, Avenida del Hospicio, S/N, 18010 Granada, Spain
| | | | - Susana Agustí
- Red Sea Research Center, Division of Biological and Environmental Sciences and Engineering, King Abdullah University of Science and Technology, Thuwal 23955-6900, Saudi Arabia
| | - Marta Estrada
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Josep M. Gasol
- Departament de Biologia Marina i Oceanografia, Institut de Ciències del Mar, Consell Superior d’Investigacions Científiques (ICM-CSIC), Passeig Marítim de la Barceloneta 37-49, 08003 Barcelona, Catalunya, Spain
| | - Carlos M. Duarte
- Red Sea Research Center, Division of Biological and Environmental Sciences and Engineering, King Abdullah University of Science and Technology, Thuwal 23955-6900, Saudi Arabia
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8
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Morán XAG, Gasol JM, Pernice MC, Mangot JF, Massana R, Lara E, Vaqué D, Duarte CM. Temperature regulation of marine heterotrophic prokaryotes increases latitudinally as a breach between bottom-up and top-down controls. GLOBAL CHANGE BIOLOGY 2017; 23:3956-3964. [PMID: 28423463 DOI: 10.1111/gcb.13730] [Citation(s) in RCA: 22] [Impact Index Per Article: 3.1] [Reference Citation Analysis] [Abstract] [Key Words] [MESH Headings] [Track Full Text] [Subscribe] [Scholar Register] [Received: 12/04/2016] [Accepted: 04/07/2017] [Indexed: 06/07/2023]
Abstract
Planktonic heterotrophic prokaryotes make up the largest living biomass and process most organic matter in the ocean. Determining when and where the biomass and activity of heterotrophic prokaryotes are controlled by resource availability (bottom-up), predation and viral lysis (top-down) or temperature will help in future carbon cycling predictions. We conducted an extensive survey across subtropical and tropical waters of the Atlantic, Indian and Pacific Oceans during the Malaspina 2010 Global Circumnavigation Expedition and assessed indices for these three types of controls at 109 stations (mostly from the surface to 4,000 m depth). Temperature control was approached by the apparent activation energy in eV (ranging from 0.46 to 3.41), bottom-up control by the slope of the log-log relationship between biomass and production rate (ranging from -0.12 to 1.09) and top-down control by an index that considers the relative abundances of heterotrophic nanoflagellates and viruses (ranging from 0.82 to 4.83). We conclude that temperature becomes dominant (i.e. activation energy >1.5 eV) within a narrow window of intermediate values of bottom-up (0.3-0.6) and top-down 0.8-1.2) controls. A pervasive latitudinal pattern of decreasing temperature regulation towards the Equator, regardless of the oceanic basin, suggests that the impact of global warming on marine microbes and their biogeochemical function will be more intense at higher latitudes. Our analysis predicts that 1°C ocean warming will result in increased biomass of heterotrophic prokaryoplankton only in waters with <26°C of mean annual surface temperature.
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Affiliation(s)
- Xosé Anxelu G Morán
- Biological and Environmental Sciences and Engineering Division (BESE), Red Sea Research Center, King Abdullah University of Science and Technology (KAUST), Thuwal, Saudi Arabia
| | - Josep M Gasol
- Institut de Ciències del Mar, CSIC, Barcelona, Catalonia, Spain
| | - Massimo C Pernice
- Institut de Ciències del Mar, CSIC, Barcelona, Catalonia, Spain
- University of Stockholm, Stockholm, Sweden
| | | | - Ramon Massana
- Institut de Ciències del Mar, CSIC, Barcelona, Catalonia, Spain
| | - Elena Lara
- Institut de Ciències del Mar, CSIC, Barcelona, Catalonia, Spain
| | - Dolors Vaqué
- Institut de Ciències del Mar, CSIC, Barcelona, Catalonia, Spain
| | - Carlos M Duarte
- Biological and Environmental Sciences and Engineering Division (BESE), Red Sea Research Center, King Abdullah University of Science and Technology (KAUST), Thuwal, Saudi Arabia
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