Deep-Water Chemosynthetic Ecosystem Research during the Census of Marine Life Decade and Beyond: A Proposed Deep-Ocean Road Map
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{"title"=>"Deep-water chemosynthetic ecosystem research during the census of marine life decade and beyond: A proposed deep-ocean road map", "type"=>"journal", "authors"=>[{"first_name"=>"Christopher R.", "last_name"=>"German", "scopus_author_id"=>"7004994297"}, {"first_name"=>"Eva", "last_name"=>"Ramirez-Llodra", "scopus_author_id"=>"6506434915"}, {"first_name"=>"Maria C.", "last_name"=>"Baker", "scopus_author_id"=>"7403075121"}, {"first_name"=>"Paul A.", "last_name"=>"Tyler", "scopus_author_id"=>"7102921991"}, {"first_name"=>"Amy", "last_name"=>"Baco-Taylor", "scopus_author_id"=>"26664405700"}, {"first_name"=>"Antje", "last_name"=>"Boetius", "scopus_author_id"=>"6701454625"}, {"first_name"=>"Monika", "last_name"=>"Bright", "scopus_author_id"=>"7005055304"}, {"first_name"=>"Lucia Campos", "last_name"=>"de Siqueira", "scopus_author_id"=>"57195466062"}, {"first_name"=>"Erik E.", "last_name"=>"Cordes", "scopus_author_id"=>"7003967049"}, {"first_name"=>"Daniel", "last_name"=>"Desbruyères", "scopus_author_id"=>"55951191600"}, {"first_name"=>"Nicole", "last_name"=>"Dubilier", "scopus_author_id"=>"55903373000"}, {"first_name"=>"Charles R.", "last_name"=>"Fisher", "scopus_author_id"=>"7402130084"}, {"first_name"=>"Yoshihiro", "last_name"=>"Fujiwara", "scopus_author_id"=>"35275024500"}, {"first_name"=>"Françoise", "last_name"=>"Gaill", "scopus_author_id"=>"35579738100"}, {"first_name"=>"Andrey", "last_name"=>"Gebruk", "scopus_author_id"=>"6603354750"}, {"first_name"=>"Kim", "last_name"=>"Juniper", "scopus_author_id"=>"6701682665"}, {"first_name"=>"Lisa A.", "last_name"=>"Levin", "scopus_author_id"=>"7202247083"}, {"first_name"=>"P. A.", "last_name"=>"Lokabharathi", "scopus_author_id"=>"6505669290"}, {"first_name"=>"Anna", "last_name"=>"Metaxas", "scopus_author_id"=>"7006356746"}, {"first_name"=>"Ashley A.", "last_name"=>"Rowden", "scopus_author_id"=>"7004209869"}, {"first_name"=>"Ricardo S.", "last_name"=>"Santos", "scopus_author_id"=>"7201375289"}, {"first_name"=>"Tim M.", "last_name"=>"Shank", "scopus_author_id"=>"6701526032"}, {"first_name"=>"Craig R.", "last_name"=>"Smith", "scopus_author_id"=>"7501648696"}, {"first_name"=>"Cindy L.", "last_name"=>"Van Dover", "scopus_author_id"=>"7005034079"}, {"first_name"=>"Craig M.", "last_name"=>"Young", "scopus_author_id"=>"7403445953"}, {"first_name"=>"Anders", "last_name"=>"Warén", "scopus_author_id"=>"6701925524"}], "year"=>2011, "source"=>"PLoS ONE", "identifiers"=>{"pui"=>"362284921", "sgr"=>"79961145574", "issn"=>"19326203", "arxiv"=>"10.1371/journal.pone.0023259", "pmid"=>"21829722", "scopus"=>"2-s2.0-79961145574", "doi"=>"10.1371/journal.pone.0023259", "isbn"=>"1932-6203"}, "id"=>"df845818-ab92-3de7-8469-3d2cc916b8fb", "abstract"=>"The ChEss project of the Census of Marine Life (2002-2010) helped foster internationally-coordinated studies worldwide focusing on exploration for, and characterization of new deep-sea chemosynthetic ecosystem sites. This work has advanced our understanding of the nature and factors controlling the biogeography and biodiversity of these ecosystems in four geographic locations: the Atlantic Equatorial Belt (AEB), the New Zealand region, the Arctic and Antarctic and the SE Pacific off Chile. In the AEB, major discoveries include hydrothermal seeps on the Costa Rica margin, deepest vents found on the Mid-Cayman Rise and the hottest vents found on the Southern Mid-Atlantic Ridge. It was also shown that the major fracture zones on the MAR do not create barriers for the dispersal but may act as trans-Atlantic conduits for larvae. In New Zealand, investigations of a newly found large cold-seep area suggest that this region may be a new biogeographic province. In the Arctic, the newly discovered sites on the Mohns Ridge (71°N) showed extensive mats of sulfur-oxidisng bacteria, but only one gastropod potentially bears chemosynthetic symbionts, while cold seeps on the Haakon Mossby Mud Volcano (72°N) are dominated by siboglinid worms. In the Antarctic region, the first hydrothermal vents south of the Polar Front were located and biological results indicate that they may represent a new biogeographic province. The recent exploration of the South Pacific region has provided evidence for a sediment hosted hydrothermal source near a methane-rich cold-seep area. Based on our 8 years of investigations of deep-water chemosynthetic ecosystems worldwide, we suggest highest priorities for future research: (i) continued exploration of the deep-ocean ridge-crest; (ii) increased focus on anthropogenic impacts; (iii) concerted effort to coordinate a major investigation of the deep South Pacific Ocean - the largest contiguous habitat for life within Earth's biosphere, but also the world's least investigated deep-ocean basin.", "link"=>"http://www.mendeley.com/research/deepwater-chemosynthetic-ecosystem-research-during-census-marine-life-decade-beyond-proposed-deepoce", "reader_count"=>131, "reader_count_by_academic_status"=>{"Unspecified"=>6, "Professor > Associate Professor"=>8, "Researcher"=>28, "Student > Doctoral Student"=>7, "Student > Ph. D. 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Student"=>32, "Student > Postgraduate"=>4, "Student > Master"=>22, "Other"=>6, "Student > Bachelor"=>9, "Lecturer"=>4, "Professor"=>5}, "reader_count_by_subject_area"=>{"Unspecified"=>11, "Engineering"=>1, "Environmental Science"=>20, "Biochemistry, Genetics and Molecular Biology"=>2, "Agricultural and Biological Sciences"=>65, "Neuroscience"=>1, "Pharmacology, Toxicology and Pharmaceutical Science"=>1, "Chemical Engineering"=>1, "Social Sciences"=>3, "Immunology and Microbiology"=>2, "Earth and Planetary Sciences"=>24}, "reader_count_by_subdiscipline"=>{"Engineering"=>{"Engineering"=>1}, "Neuroscience"=>{"Neuroscience"=>1}, "Social Sciences"=>{"Social Sciences"=>3}, "Immunology and Microbiology"=>{"Immunology and Microbiology"=>2}, "Earth and Planetary Sciences"=>{"Earth and Planetary Sciences"=>24}, "Agricultural and Biological Sciences"=>{"Agricultural and Biological Sciences"=>65}, "Biochemistry, Genetics and Molecular Biology"=>{"Biochemistry, Genetics and Molecular Biology"=>2}, "Unspecified"=>{"Unspecified"=>11}, "Environmental Science"=>{"Environmental Science"=>20}, "Pharmacology, Toxicology and Pharmaceutical Science"=>{"Pharmacology, Toxicology and Pharmaceutical Science"=>1}, "Chemical Engineering"=>{"Chemical Engineering"=>1}}, "reader_count_by_country"=>{"Canada"=>1, "United States"=>4, "Poland"=>1, "Brazil"=>2, "Italy"=>1, "United Kingdom"=>2, "Mexico"=>1, "Australia"=>1, "Chile"=>1, "Portugal"=>1, "India"=>1}, "group_count"=>3}

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  • {"files"=>["https://ndownloader.figshare.com/files/749148"], "description"=>"<p>A) The Beebe Vent, Piccard Hydrothermal Field on the Mid-Cayman Rise (4960 m depth), image taken by HyBIS during Voyage 44 of the RRS James Cook, April 2010 (© Jon Copley, University of Southampton/NOCS) (Connelly et al,. 2011); B, Turtle Pits hydrothermal vent, first vents discovered on the South MAR, 2005 (© ROV Quest, Marum, Bremen); C, Bubbylon hydrothermal vents on the North MAR discovered near the Azores in October 2010 (© ROV Quest, Marum, Bremen); D, Black smokers on the East Scotia Ridge south of the Polar Front discovered in January 2009 (©Paul Tyler and Jon Copley, ChEsSo Consortium, University of Southampton, UK, ROV Isis).</p>", "links"=>[], "tags"=>["discovered", "deep-water", "chemosynthetic", "habitats"], "article_id"=>419518, "categories"=>["Inorganic Chemistry", "Ecology"], "users"=>["Christopher R. German", "Eva Ramirez-Llodra", "Maria C. Baker", "Paul A. Tyler"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0023259.g003", "stats"=>{"downloads"=>2, "page_views"=>13, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Photos_showing_some_of_the_newly_discovered_deep_water_chemosynthetic_habitats_found_during_ChEss_/419518", "title"=>"Photos showing some of the newly discovered deep-water chemosynthetic habitats found during ChEss.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2013-02-20 16:01:47"}
  • {"files"=>["https://ndownloader.figshare.com/files/748850"], "description"=>"<p>Central map: global map showing the mid-ocean ridge and the known hydrothermal vent provinces (colour dots) known in 2002 (map modified from Van Dover et al., 2002). Highlighted regions indicate the ChEss field program areas, with priority areas (pink) and secondary areas (yellow). Priority areas: A) Atlantic Equatorial Belt; B) New Zealand region, C1) Arctic Ocean, C2) Antarctic region; D) South East Pacific/Chile Triple-Junction; Secondary areas: (a) MAR north of Iceland; (b) MAR north of Azores; (c) Brazilian margin; (d) Eastern Mediterranean; (f) SW Indian Ridge; (g) Central Indian Ridge. Arrows point to detailed maps of each priority field program area. A) AEB: (1) Equatorial MAR and fracture zones; (2) Mid-Cayman Rise; (3) Gulf of Mexico; (4) Barbados Accretionary Prism; (5) NW African margin; (6), Costa Rica margin. B) New Zealand (1) Kermadec Arc; (2) Hikurangi margin; (3) Otago margin; (4) South Island fjords. C1) Arctic basin: (1) Gakkel Ridge. C2) East Scotia Ridge, Southern Ocean: (1) E9 area; (2) E2 area; (3) Bransfield Strait. D) South East Pacific/Chile Triple Junction: (1) East Chile Rise; (2) Chile margin.</p>", "links"=>[], "tags"=>["ecology", "marine and aquatic sciences"], "article_id"=>419226, "categories"=>["Inorganic Chemistry", "Ecology"], "users"=>["Christopher R. German", "Eva Ramirez-Llodra", "Maria C. Baker", "Paul A. Tyler"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0023259.g001", "stats"=>{"downloads"=>3, "page_views"=>16, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_ChEss_field_program_areas_/419226", "title"=>"ChEss field program areas.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2013-02-20 16:00:09"}
  • {"files"=>["https://ndownloader.figshare.com/files/749497"], "description"=>"<p>*HFI: Hurlbert's First Index is a sample-size independent proxy for species richness. Here, colours (red = high) show predicted numbers of distinct species in a random sample of 50 observations; white: areas still awaiting collection of 50+ observations!</p>", "links"=>[], "tags"=>["biodiversity", "pacific", "separated", "areas", "devoid"], "article_id"=>419869, "categories"=>["Inorganic Chemistry", "Ecology"], "users"=>["Christopher R. German", "Eva Ramirez-Llodra", "Maria C. Baker", "Paul A. Tyler"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0023259.g005", "stats"=>{"downloads"=>2, "page_views"=>93, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_HFI_map_www_coml_org_showing_how_biodiversity_hot_spots_to_West_and_East_in_the_South_Pacific_are_separated_by_areas_devoid_of_data_/419869", "title"=>"HFI* map (www.coml.org) showing how biodiversity “hot-spots” to West and East in the South Pacific are separated by areas devoid of data.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2013-02-20 16:03:40"}
  • {"files"=>["https://ndownloader.figshare.com/files/749807"], "description"=>"<p>Areas of interest to any of the 7 sub-disciplines represented among the workshop participants (InterRidge Long Range Exploration working group, 2010 workshop, NOCS, UK) were first identified by ticks. Each disciplinary group then assigned highest prioritization to 5 key areas (marked as 1). Total indicates the number of high priority hits for each geographic area.</p>", "links"=>[], "tags"=>["areas", "internationally", "coordinated", "mid-ocean"], "article_id"=>420184, "categories"=>["Inorganic Chemistry", "Ecology"], "users"=>["Christopher R. German", "Eva Ramirez-Llodra", "Maria C. Baker", "Paul A. Tyler"], "doi"=>"https://dx.doi.org/10.1 371/journal.pone.0023259.t001", "stats"=>{"downloads"=>3, "page_views"=>4, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Geographic_areas_of_interest_for_the_next_decade_of_internationally_coordinated_mid_ocean_ridge_research_/420184", "title"=>"Geographic areas of interest for the next decade of internationally coordinated mid-ocean ridge research.", "pos_in_sequence"=>0, "defined_type"=>3, "published_date"=>"2013-02-20 16:05:15"}
  • {"files"=>["https://ndownloader.figshare.com/files/749011"], "description"=>"<p>Created by M Baker and D Cuvelier, using site location data gathered from published literature or provided by researchers.</p>", "links"=>[], "tags"=>["hydrothermal", "vent", "seep", "sites", "been", "studied"], "article_id"=>419382, "categories"=>["Inorganic Chemistry", "Ecology"], "users"=>["Christopher R. German", "Eva Ramirez-Llodra", "Maria C. Baker", "Paul A. Tyler"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0023259.g002", "stats"=>{"downloads"=>18, "page_views"=>176, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Global_distribution_of_hydrothermal_vent_red_cold_seep_blue_and_whale_fall_yellow_sites_that_have_been_studied_with_respect_to_their_fauna_/419382", "title"=>"Global distribution of hydrothermal vent (red), cold seep (blue) and whale fall (yellow) sites that have been studied with respect to their fauna.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2013-02-20 16:01:01"}
  • {"files"=>["https://ndownloader.figshare.com/files/749676"], "description"=>"<p>1, Tonga-Kermadec arc; 2, deep-ocean trenches; (3) mid-plate seamounts of the Louisville Ridge; 4 & 6, Pacific-Antarctic Ridge; 5 & 8, abyssal plains; 7, Southern EPR; 9, Chile margin; 10, Bransfield Strait back-arc basin.</p>", "links"=>[], "tags"=>["pacific", "numbered", "locations"], "article_id"=>420051, "categories"=>["Inorganic Chemistry", "Ecology"], "users"=>["Christopher R. German", "Eva Ramirez-Llodra", "Maria C. Baker", "Paul A. Tyler"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0023259.g006", "stats"=>{"downloads"=>3, "page_views"=>9, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Bathymetric_projection_of_the_South_Pacific_Ocean_with_numbered_field_locations_as_described_in_the_text_/420051", "title"=>"Bathymetric projection of the South Pacific Ocean with numbered field locations as described in the text.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2013-02-20 16:04:38"}
  • {"files"=>["https://ndownloader.figshare.com/files/749351"], "description"=>"<p>Ellipses show three categories of importance assigned to twenty three separate locations distributed along the ridge axis (see <a href=\"http://www.plosone.org/article/info:doi/10.1371/journal.pone.0023259#pone-0023259-t001\" target=\"_blank\">Table 1</a>); different coloured lines along-axis represent regions that share many of the same species (see Van Dover, 2010).</p>", "links"=>[], "tags"=>["illustrating", "biogeographic", "differentiation", "invertebrate", "hydrothermal", "vents", "regions", "ridge-crest"], "article_id"=>419713, "categories"=>["Inorganic Chemistry", "Ecology"], "users"=>["Christopher R. German", "Eva Ramirez-Llodra", "Maria C. Baker", "Paul A. Tyler"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0023259.g004", "stats"=>{"downloads"=>6, "page_views"=>119, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Annotated_map_after_Van_Dover_2010_of_the_global_ridge_crest_illustrating_both_a_model_of_the_global_biogeographic_differentiation_of_invertebrate_species_associated_with_hydrothermal_vents_and_regions_recently_identified_by_the_international_community_a/419713", "title"=>"Annotated map (after Van Dover, 2010) of the global ridge crest, illustrating both a model of the global biogeographic differentiation of invertebrate species associated with hydrothermal vents and regions recently identified by the international community as being of continuing importance for future ridge-crest exploration.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2013-02-20 16:02:48"}

PMC Usage Stats | Further Information

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