Living Benthic Foraminifera from the Surface and Subsurface Sediment Layers Applied to the Environmental Characterization of the Brazilian Continental Slope (SW Atlantic)
Living benthic foraminifera (>63 µm) were studied to characterize the continental slope of the Potiguar Basin (SW Atlantic). Foraminifers from the surface (0–2 cm), subsurface (2–5 cm), and integrated (0–5 cm) sediment layers were analyzed to verify their contribution to environmental characteriz...
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Veröffentlicht in: | Water (Basel) 2021-07, Vol.13 (13), p.1863 |
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creator | Santa-Rosa, Luciana Cristina de Carvalho Disaró, Sibelle Trevisan Totah, Violeta Watanabe, Silvia Guimarães, Ana Tereza Bittencourt |
description | Living benthic foraminifera (>63 µm) were studied to characterize the continental slope of the Potiguar Basin (SW Atlantic). Foraminifers from the surface (0–2 cm), subsurface (2–5 cm), and integrated (0–5 cm) sediment layers were analyzed to verify their contribution to environmental characterization. It was also estimated if and which changes occur when the subsurface is added. Sampling stations were distributed in five transects in four isobaths (150, 400, 1000, and 2000 m). Sediment samples were fixed with 4% buffered formaldehyde and stained with Bengal rose. Were recorded 396 species in the surface layer, 228 in the subsurface, and 449 in integrating both layers. This study did not include tubular agglutinated species. The assemblages from 150 m isobath indicated the upper slope, from 400 m indicated the middle slope and the ones from the 2000 m indicated the lower slope. The surface layer’s assemblage at 1000 m isobath was more similar to the middle slope; in contrast, its subsurface layer’s assemblage had more similarity with the lower slope. Rarefaction curves, Permanova, and NMDS routines indicated a high resemblance between surface and integrated layers. Therefore, the first two centimeters were sufficient to characterize this region based on living benthic foraminifera. |
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Foraminifers from the surface (0–2 cm), subsurface (2–5 cm), and integrated (0–5 cm) sediment layers were analyzed to verify their contribution to environmental characterization. It was also estimated if and which changes occur when the subsurface is added. Sampling stations were distributed in five transects in four isobaths (150, 400, 1000, and 2000 m). Sediment samples were fixed with 4% buffered formaldehyde and stained with Bengal rose. Were recorded 396 species in the surface layer, 228 in the subsurface, and 449 in integrating both layers. This study did not include tubular agglutinated species. The assemblages from 150 m isobath indicated the upper slope, from 400 m indicated the middle slope and the ones from the 2000 m indicated the lower slope. The surface layer’s assemblage at 1000 m isobath was more similar to the middle slope; in contrast, its subsurface layer’s assemblage had more similarity with the lower slope. Rarefaction curves, Permanova, and NMDS routines indicated a high resemblance between surface and integrated layers. Therefore, the first two centimeters were sufficient to characterize this region based on living benthic foraminifera.</description><identifier>ISSN: 2073-4441</identifier><identifier>EISSN: 2073-4441</identifier><identifier>DOI: 10.3390/w13131863</identifier><language>eng</language><publisher>Basel: MDPI AG</publisher><subject>Continental slope ; Habitats ; Museums ; Ocean circulation ; Rarefaction ; Salinity ; Sediment samplers ; Sediments ; Surface layers</subject><ispartof>Water (Basel), 2021-07, Vol.13 (13), p.1863</ispartof><rights>2021 by the authors. Licensee MDPI, Basel, Switzerland. This article is an open access article distributed under the terms and conditions of the Creative Commons Attribution (CC BY) license (https://creativecommons.org/licenses/by/4.0/). 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Foraminifers from the surface (0–2 cm), subsurface (2–5 cm), and integrated (0–5 cm) sediment layers were analyzed to verify their contribution to environmental characterization. It was also estimated if and which changes occur when the subsurface is added. Sampling stations were distributed in five transects in four isobaths (150, 400, 1000, and 2000 m). Sediment samples were fixed with 4% buffered formaldehyde and stained with Bengal rose. Were recorded 396 species in the surface layer, 228 in the subsurface, and 449 in integrating both layers. This study did not include tubular agglutinated species. The assemblages from 150 m isobath indicated the upper slope, from 400 m indicated the middle slope and the ones from the 2000 m indicated the lower slope. The surface layer’s assemblage at 1000 m isobath was more similar to the middle slope; in contrast, its subsurface layer’s assemblage had more similarity with the lower slope. Rarefaction curves, Permanova, and NMDS routines indicated a high resemblance between surface and integrated layers. Therefore, the first two centimeters were sufficient to characterize this region based on living benthic foraminifera.</description><subject>Continental slope</subject><subject>Habitats</subject><subject>Museums</subject><subject>Ocean circulation</subject><subject>Rarefaction</subject><subject>Salinity</subject><subject>Sediment samplers</subject><subject>Sediments</subject><subject>Surface layers</subject><issn>2073-4441</issn><issn>2073-4441</issn><fulltext>true</fulltext><rsrctype>article</rsrctype><creationdate>2021</creationdate><recordtype>article</recordtype><sourceid>ABUWG</sourceid><sourceid>AFKRA</sourceid><sourceid>AZQEC</sourceid><sourceid>BENPR</sourceid><sourceid>CCPQU</sourceid><sourceid>DWQXO</sourceid><recordid>eNpNkU1PwzAMhisEEtPYgX8QiQs7DNom_chxmzZAmsShII6VkzosU5eUNBvafhK_ku5DCPvg19bz2gcHwW0UPlDKw8fviHaZp_Qi6MVhRkeMsejyn74OBm27CrtgPM-TsBf8LPRWm08yQeOXWpK5dbDWRit0QJSza-KXSIqNUyCRgKk6LdpzW2Cl152RLGCHriXjpqk1VsTbo2tmttpZcyCgJtMlOJAend6D19YQq47UxMFe1xoMmVrjtTnRRW0bJPfFBxn7Grq5HN4EVwrqFgfn2g_e57O36fNo8fr0Mh0vRjLmsR-ByCsVVYpJpBkTyLmEkDNBGeNJlrA0SjMZS5VQxTERaYaVgCoSeS4SBIG0H9yd9jbOfm2w9eXKbpzpTpZxwngWZnlEO2p4oqSzbetQlY3Ta3C7MgrLwzfKv2_QX6cNf6I</recordid><startdate>20210701</startdate><enddate>20210701</enddate><creator>Santa-Rosa, Luciana Cristina de Carvalho</creator><creator>Disaró, Sibelle Trevisan</creator><creator>Totah, Violeta</creator><creator>Watanabe, Silvia</creator><creator>Guimarães, Ana Tereza Bittencourt</creator><general>MDPI AG</general><scope>AAYXX</scope><scope>CITATION</scope><scope>ABUWG</scope><scope>AFKRA</scope><scope>AZQEC</scope><scope>BENPR</scope><scope>CCPQU</scope><scope>DWQXO</scope><scope>PIMPY</scope><scope>PQEST</scope><scope>PQQKQ</scope><scope>PQUKI</scope><scope>PRINS</scope><orcidid>https://orcid.org/0000-0002-3633-6484</orcidid></search><sort><creationdate>20210701</creationdate><title>Living Benthic Foraminifera from the Surface and Subsurface Sediment Layers Applied to the Environmental Characterization of the Brazilian Continental Slope (SW Atlantic)</title><author>Santa-Rosa, Luciana Cristina de Carvalho ; Disaró, Sibelle Trevisan ; Totah, Violeta ; Watanabe, Silvia ; Guimarães, Ana Tereza Bittencourt</author></sort><facets><frbrtype>5</frbrtype><frbrgroupid>cdi_FETCH-LOGICAL-c292t-ab8df1df4ce374be99ca094b344957546167c2cf53f9e5b67edbad1b88b5eabe3</frbrgroupid><rsrctype>articles</rsrctype><prefilter>articles</prefilter><language>eng</language><creationdate>2021</creationdate><topic>Continental slope</topic><topic>Habitats</topic><topic>Museums</topic><topic>Ocean circulation</topic><topic>Rarefaction</topic><topic>Salinity</topic><topic>Sediment samplers</topic><topic>Sediments</topic><topic>Surface layers</topic><toplevel>peer_reviewed</toplevel><toplevel>online_resources</toplevel><creatorcontrib>Santa-Rosa, Luciana Cristina de Carvalho</creatorcontrib><creatorcontrib>Disaró, Sibelle Trevisan</creatorcontrib><creatorcontrib>Totah, Violeta</creatorcontrib><creatorcontrib>Watanabe, Silvia</creatorcontrib><creatorcontrib>Guimarães, Ana Tereza Bittencourt</creatorcontrib><collection>CrossRef</collection><collection>ProQuest Central (Alumni Edition)</collection><collection>ProQuest Central UK/Ireland</collection><collection>ProQuest Central Essentials</collection><collection>ProQuest Central</collection><collection>ProQuest One Community College</collection><collection>ProQuest Central Korea</collection><collection>Publicly Available Content Database</collection><collection>ProQuest One Academic Eastern Edition (DO NOT USE)</collection><collection>ProQuest One Academic</collection><collection>ProQuest One Academic UKI Edition</collection><collection>ProQuest Central China</collection><jtitle>Water (Basel)</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Santa-Rosa, Luciana Cristina de Carvalho</au><au>Disaró, Sibelle Trevisan</au><au>Totah, Violeta</au><au>Watanabe, Silvia</au><au>Guimarães, Ana Tereza Bittencourt</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Living Benthic Foraminifera from the Surface and Subsurface Sediment Layers Applied to the Environmental Characterization of the Brazilian Continental Slope (SW Atlantic)</atitle><jtitle>Water (Basel)</jtitle><date>2021-07-01</date><risdate>2021</risdate><volume>13</volume><issue>13</issue><spage>1863</spage><pages>1863-</pages><issn>2073-4441</issn><eissn>2073-4441</eissn><abstract>Living benthic foraminifera (>63 µm) were studied to characterize the continental slope of the Potiguar Basin (SW Atlantic). Foraminifers from the surface (0–2 cm), subsurface (2–5 cm), and integrated (0–5 cm) sediment layers were analyzed to verify their contribution to environmental characterization. It was also estimated if and which changes occur when the subsurface is added. Sampling stations were distributed in five transects in four isobaths (150, 400, 1000, and 2000 m). Sediment samples were fixed with 4% buffered formaldehyde and stained with Bengal rose. Were recorded 396 species in the surface layer, 228 in the subsurface, and 449 in integrating both layers. This study did not include tubular agglutinated species. The assemblages from 150 m isobath indicated the upper slope, from 400 m indicated the middle slope and the ones from the 2000 m indicated the lower slope. The surface layer’s assemblage at 1000 m isobath was more similar to the middle slope; in contrast, its subsurface layer’s assemblage had more similarity with the lower slope. 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subjects | Continental slope Habitats Museums Ocean circulation Rarefaction Salinity Sediment samplers Sediments Surface layers |
title | Living Benthic Foraminifera from the Surface and Subsurface Sediment Layers Applied to the Environmental Characterization of the Brazilian Continental Slope (SW Atlantic) |
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