Macrobenthic Biomass Relations in the Faroe-Shetland Channel: An Arctic-Atlantic Boundary Environment
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{"title"=>"Macrobenthic biomass relations in the faroe-shetland channel: An Arctic-Atlantic boundary environment", "type"=>"journal", "authors"=>[{"first_name"=>"Bhavani E.", "last_name"=>"Narayanaswamy", "scopus_author_id"=>"6506960170"}, {"first_name"=>"Brian J.", "last_name"=>"Bett", "scopus_author_id"=>"7003633211"}], "year"=>2011, "source"=>"PLoS ONE", "identifiers"=>{"pmid"=>"21526171", "sgr"=>"79955528471", "doi"=>"10.1371/journal.pone.0018602", "scopus"=>"2-s2.0-79955528471", "pui"=>"361682389", "issn"=>"19326203"}, "id"=>"ecb15cd3-f120-3381-86bb-33dda6f1be91", "abstract"=>"The Faroe-Shetland Channel, located in the NE Atlantic, ranges in depth from 0-1700 m and is an unusual deep-sea environment because of its complex and dynamic hydrographic regime, as well as having numerous different seafloor habitats. Macrofaunal samples have been collected on a 0.5 mm mesh sieve from over 300 stations in a wide area survey and on nested 0.5 and 0.25 mm mesh sieves along a specific depth transect. Contrary to general expectation, macrofauanl biomass in the Channel did not decline with increasing depth. When examined at phylum level, two main biomass patterns with depth were apparent: (a) polychaetes showed little change in biomass on the upper slope then increased markedly below 500 m to a depth of 1100 m before declining; and (b) other phyla showed enhanced biomass between 300-500 m. The polychaete response may be linked with a seafloor environment change to relatively quiescent hydrodynamic conditions and an increasing sediment mud content that occurs at c. 500 m. In contrast, the mid-slope enhancement of other phyla biomass may reflect the hydrodynamically active interface between the warm and cold water masses present in the Channel at c. 300-500 m. Again contrary to expectation, mean macrofaunal body size did not decline with depth, and the relative contribution of smaller (>0.25 mm<0.5 mm) to total (>0.25 mm) macrobenthos did not increase with depth. Overall our total biomass and average individual biomass estimates appear to be greater than those predicted from global analyses. It is clear that global models of benthic biomass distribution may mask significant variations at the local and regional scale.", "link"=>"http://www.mendeley.com/research/macrobenthic-biomass-relations-faroeshetland-channel-arcticatlantic-boundary-environment", "reader_count"=>27, "reader_count_by_academic_status"=>{"Unspecified"=>1, "Professor > Associate Professor"=>2, "Researcher"=>8, "Student > Ph. D. Student"=>8, "Student > Postgraduate"=>1, "Student > Master"=>4, "Other"=>1, "Student > Bachelor"=>2}, "reader_count_by_user_role"=>{"Unspecified"=>1, "Professor > Associate Professor"=>2, "Researcher"=>8, "Student > Ph. D. Student"=>8, "Student > Postgraduate"=>1, "Student > Master"=>4, "Other"=>1, "Student > Bachelor"=>2}, "reader_count_by_subject_area"=>{"Unspecified"=>2, "Environmental Science"=>9, "Agricultural and Biological Sciences"=>14, "Earth and Planetary Sciences"=>2}, "reader_count_by_subdiscipline"=>{"Earth and Planetary Sciences"=>{"Earth and Planetary Sciences"=>2}, "Agricultural and Biological Sciences"=>{"Agricultural and Biological Sciences"=>14}, "Unspecified"=>{"Unspecified"=>2}, "Environmental Science"=>{"Environmental Science"=>9}}, "reader_count_by_country"=>{"United Kingdom"=>6, "Russia"=>1}, "group_count"=>1}

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  • {"files"=>["https://ndownloader.figshare.com/files/781187"], "description"=>"<p>(A) Density. (B) Biomass.</p>", "links"=>[], "tags"=>["biomass", "mm", "fractions", "transect"], "article_id"=>451565, "categories"=>["Inorganic Chemistry"], "users"=>["Bhavani E. Narayanaswamy", "Brian J. Bett"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0018602.g005", "stats"=>{"downloads"=>1, "page_views"=>4, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Corrected_density_and_biomass_values_of_the_gt_0_25_mm_lt_0_5_mm_and_gt_0_25_mm_fractions_for_the_transect_stations_/451565", "title"=>"Corrected density and biomass values of the >0.25 mm<0.5 mm and >0.25 mm fractions for the transect stations.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2011-04-22 00:26:05"}
  • {"files"=>["https://ndownloader.figshare.com/files/781057"], "description"=>"<p>Wide-area survey geometric mean biomass (>0.5 mm, corrected) of selected major taxa, shown after depth-ordered smoothing (4253H, twice method; see e.g. Velleman <a href=\"http://www.plosone.org/article/info:doi/10.1371/journal.pone.0018602#pone.0018602-Velleman1\" target=\"_blank\">[53]</a>).</p>", "links"=>[], "tags"=>["depth-related", "patterns", "macrofaunal", "biomass"], "article_id"=>451432, "categories"=>["Inorganic Chemistry"], "users"=>["Bhavani E. Narayanaswamy", "Brian J. Bett"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0018602.g004", "stats"=>{"downloads"=>7, "page_views"=>7, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Summary_of_depth_related_patterns_in_macrofaunal_biomass_distribution_with_depth_/451432", "title"=>"Summary of depth-related patterns in macrofaunal biomass distribution with depth.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2011-04-22 00:23:52"}
  • {"files"=>["https://ndownloader.figshare.com/files/391596"], "description"=>"<div><p>The Faroe-Shetland Channel, located in the NE Atlantic, ranges in depth from 0–1700 m and is an unusual deep-sea environment because of its complex and dynamic hydrographic regime, as well as having numerous different seafloor habitats. Macrofaunal samples have been collected on a 0.5 mm mesh sieve from over 300 stations in a wide area survey and on nested 0.5 and 0.25 mm mesh sieves along a specific depth transect. Contrary to general expectation, macrofauanl biomass in the Channel did not decline with increasing depth. When examined at phylum level, two main biomass patterns with depth were apparent: (a) polychaetes showed little change in biomass on the upper slope then increased markedly below 500 m to a depth of 1100 m before declining; and (b) other phyla showed enhanced biomass between 300–500 m. The polychaete response may be linked with a seafloor environment change to relatively quiescent hydrodynamic conditions and an increasing sediment mud content that occurs at c. 500 m. In contrast, the mid-slope enhancement of other phyla biomass may reflect the hydrodynamically active interface between the warm and cold water masses present in the Channel at c. 300–500 m. Again contrary to expectation, mean macrofaunal body size did not decline with depth, and the relative contribution of smaller (>0.25 mm<0.5 mm) to total (>0.25 mm) macrobenthos did not increase with depth. Overall our total biomass and average individual biomass estimates appear to be greater than those predicted from global analyses. It is clear that global models of benthic biomass distribution may mask significant variations at the local and regional scale.</p> </div>", "links"=>[], "tags"=>["macrobenthic", "biomass", "relations", "faroe-shetland", "arctic-atlantic"], "article_id"=>137333, "categories"=>["Inorganic Chemistry"], "users"=>["Bhavani E. Narayanaswamy", "Brian J. Bett"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0018602", "stats"=>{"downloads"=>4, "page_views"=>13, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/Macrobenthic_Biomass_Relations_in_the_Faroe_Shetland_Channel_An_Arctic_Atlantic_Boundary_Environment/137333", "title"=>"Macrobenthic Biomass Relations in the Faroe-Shetland Channel: An Arctic-Atlantic Boundary Environment", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2011-04-22 02:02:13"}
  • {"files"=>["https://ndownloader.figshare.com/files/781345"], "description"=>"<p>Median and interquartile range are shown for mud content.</p>", "links"=>[], "tags"=>["sediment"], "article_id"=>451720, "categories"=>["Inorganic Chemistry"], "users"=>["Bhavani E. Narayanaswamy", "Brian J. Bett"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0018602.g007", "stats"=>{"downloads"=>1, "page_views"=>3, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Variation_in_sediment_mud_content_lt_63_181_m_and_minimum_bottom_water_temperature_with_depth_/451720", "title"=>"Variation in sediment mud content (<63 µm) and minimum bottom water temperature with depth.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2011-04-22 00:28:40"}
  • {"files"=>["https://ndownloader.figshare.com/files/780501"], "description"=>"<p>Open circles represent the 329 stations sampled in the wider area survey, filled circles represent the 15 stations of the depth transect. Inset: Bottom water temperature range in the study area (see text for details).</p>", "links"=>[], "tags"=>["locations", "faroe-shetland", "sampling"], "article_id"=>450876, "categories"=>["Inorganic Chemistry"], "users"=>["Bhavani E. Narayanaswamy", "Brian J. Bett"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0018602.g001", "stats"=>{"downloads"=>1, "page_views"=>12, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Chart_showing_the_locations_of_Faroe_Shetland_Channel_sampling_sites_/450876", "title"=>"Chart showing the locations of Faroe-Shetland Channel sampling sites.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2011-04-22 00:14:36"}
  • {"files"=>["https://ndownloader.figshare.com/files/780897"], "description"=>"<p>(A) Total biomass. (B) Polychaete biomass. (C) Crustacean biomass. (D) Mollusk biomass. (E) Echinoderm biomass. (F) Other taxa biomass. Solid circles indicate the wide-area survey depth bands (geometric mean and 95% confidence interval), open circles indicate the depth transect stations (geometric mean).</p>", "links"=>[], "tags"=>["corrected", "biomass"], "article_id"=>451274, "categories"=>["Inorganic Chemistry"], "users"=>["Bhavani E. Narayanaswamy", "Brian J. Bett"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0018602.g003", "stats"=>{"downloads"=>1, "page_views"=>3, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Variation_in_corrected_biomass_gt_0_5_mm_with_depth_/451274", "title"=>"Variation in corrected biomass (>0.5 mm) with depth.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2011-04-22 00:21:14"}
  • {"files"=>["https://ndownloader.figshare.com/files/781424"], "description"=>"<p>Spearman's rank correlations of macrofaunal biomass (corrected) and environmental variables.</p>", "links"=>[], "tags"=>["correlations", "macrofaunal", "biomass"], "article_id"=>451795, "categories"=>["Inorganic Chemistry"], "users"=>["Bhavani E. Narayanaswamy", "Brian J. Bett"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0018602.t001", "stats"=>{"downloads"=>1, "page_views"=>6, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Spearman_s_rank_correlations_of_macrofaunal_biomass_corrected_and_environmental_variables_/451795", "title"=>"Spearman's rank correlations of macrofaunal biomass (corrected) and environmental variables.", "pos_in_sequence"=>0, "defined_type"=>3, "published_date"=>"2011-04-22 00:29:55"}
  • {"files"=>["https://ndownloader.figshare.com/files/780687"], "description"=>"<p>Complete wide-area survey data is shown, keyed to sampler type (MgC, Megacorer, n = 171; BC, box corer, n = 85; DG, Day grab, n = 73). (A) and (C) sample data with separate regression lines for MgC and combined BC&DG data. (B) and (D) Geometric mean and 95% confidence intervals of standing stock by sampler type irrespective of water depth.</p>", "links"=>[], "tags"=>["macrofaunal", "stocks", "faroe-shetland"], "article_id"=>451058, "categories"=>["Inorganic Chemistry"], "users"=>["Bhavani E. Narayanaswamy", "Brian J. Bett"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0018602.g002", "stats"=>{"downloads"=>1, "page_views"=>11, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Variation_in_macrofaunal_standing_stocks_gt_0_5_mm_uncorrected_with_depth_in_the_Faroe_Shetland_Channel_/451058", "title"=>"Variation in macrofaunal standing stocks (>0.5 mm, uncorrected) with depth in the Faroe-Shetland Channel.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2011-04-22 00:17:38"}
  • {"files"=>["https://ndownloader.figshare.com/files/781276"], "description"=>"<p>(A) Biomass. (B) Density. (C) Mean individual biomass. Geometric mean and 95% confidence interval are shown for each parameter (wide-area survey data). Vertical lines are the global regressions of these parameters on depth established by Rex et al. <a href=\"http://www.plosone.org/article/info:doi/10.1371/journal.pone.0018602#pone.0018602-Rex2\" target=\"_blank\">[9]</a> and Wei et al. <a href=\"http://www.plosone.org/article/info:doi/10.1371/journal.pone.0018602#pone.0018602-Wei1\" target=\"_blank\">[20]</a>.</p>", "links"=>[], "tags"=>["corrected", "macrofaunal", "biomass"], "article_id"=>451647, "categories"=>["Inorganic Chemistry"], "users"=>["Bhavani E. Narayanaswamy", "Brian J. Bett"], "doi"=>"https://dx.doi.org/10.1371/journal.pone.0018602.g006", "stats"=>{"downloads"=>3, "page_views"=>6, "likes"=>0}, "figshare_url"=>"https://figshare.com/articles/_Variation_in_corrected_macrofaunal_biomass_density_and_mean_individual_biomass_gt_0_5_mm_with_depth_/451647", "title"=>"Variation in corrected macrofaunal biomass, density and mean individual biomass (>0.5 mm) with depth.", "pos_in_sequence"=>0, "defined_type"=>1, "published_date"=>"2011-04-22 00:27:27"}

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Relative Metric

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