Seabed pockmarks associated with deepwater corals off SE Brasilian continental slope, Santos Basin

Several factors bear evidence of chemosynthetic ecosystem occurrence in the Brazilian coast; these motivated our investigation to sample three pockmarks located on the continentalslopeoffSE Brazil (26°S and 46°W) at ∼700 m depth. The crater-like features were ∼1 km in diameter and 100 m in depth, an...

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Main Authors: Sumida, Paulo Yukio Gomes, Yoshinaga, Marcos Yukio, Madureira, Lauro Antonio Saint Pastous, Hovland, Martin
Format: Article in Journal/Newspaper
Language:English
Published: 2004
Subjects:
Online Access:http://repositorio.furg.br/handle/1/3906
id ftunivfurg:oai:repositorio.furg.br:1/3906
record_format openpolar
spelling ftunivfurg:oai:repositorio.furg.br:1/3906 2023-11-12T04:06:41+01:00 Seabed pockmarks associated with deepwater corals off SE Brasilian continental slope, Santos Basin Sumida, Paulo Yukio Gomes Yoshinaga, Marcos Yukio Madureira, Lauro Antonio Saint Pastous Hovland, Martin 2004 application/pdf http://repositorio.furg.br/handle/1/3906 eng eng SUMIDA, Paulo Yukio Gomes et al. Seabed pockmarks associated with deepwater corals off SE Brasilian continental slope, Santos Basin. Marine Geology, v. 207, p. 159-167, 2004. Disponível em:<http://ac.els-cdn.com/S0025322704000726/1-s2.0-S0025322704000726-main.pdf?_tid=1afd9348408dc1d8207f207d78f93350&acdnat=1340365926_b0203db1a478ec98ab2da6af7f9a735a>. Acesso em: 22 jun. 2012. http://repositorio.furg.br/handle/1/3906 restrict access Pockmarks Deepwater corals Santos Basin SW Atlantic Ocean article 2004 ftunivfurg 2023-10-24T21:01:34Z Several factors bear evidence of chemosynthetic ecosystem occurrence in the Brazilian coast; these motivated our investigation to sample three pockmarks located on the continentalslopeoffSE Brazil (26°S and 46°W) at ∼700 m depth. The crater-like features were ∼1 km in diameter and 100 m in depth, and were identified with an echo-sounder (EK-500). They were sampled along two transects using a rectangular dredge. Our main objective was to identify possible evidence of a seep-related community. The surrounding sediments of the pockmarks seem to be filled with coral rubble harboring a rich fauna of metazoans including epilithic and chasmolithic organisms. A total of 9565 organisms were sampled. The most abundant group was the Ophiuroidea, followed by Cirripedia and Polychaeta. A number of new occurrences and new species were registered. The polychaete worm Amelinna was the first record for the Atlantic Ocean, which has been found in reducing habitats such as wood islands. The echo-sounder records also showed the presence of big deepwatercoral mounds associated with the edge of the pockmarks. These features are ∼ 20 m in height and from 180 to 360 m wide. Records of demersal fishes were also registered right above coral mounds. The presence of deepwatercoral mounds at the edge of pockmarks may be related to the flow of the cold, oxygen-rich Antarctic Intermediate Water over the bottom, or else may benefit from the fertilization of the water by the microseepage of hydrocarbons from the sediment. We suggest a more thorough survey in order to map and recognize these environments. Furthermore, our findings may shed some light on new research perspectives concerning the ecology, biogeography and evolution of reducing habitats off the Brazilian coast. Article in Journal/Newspaper Antarc* Antarctic RI FURG (Repositório da Universidade Federal do Rio Grande) Antarctic
institution Open Polar
collection RI FURG (Repositório da Universidade Federal do Rio Grande)
op_collection_id ftunivfurg
language English
topic Pockmarks
Deepwater corals
Santos Basin
SW Atlantic Ocean
spellingShingle Pockmarks
Deepwater corals
Santos Basin
SW Atlantic Ocean
Sumida, Paulo Yukio Gomes
Yoshinaga, Marcos Yukio
Madureira, Lauro Antonio Saint Pastous
Hovland, Martin
Seabed pockmarks associated with deepwater corals off SE Brasilian continental slope, Santos Basin
topic_facet Pockmarks
Deepwater corals
Santos Basin
SW Atlantic Ocean
description Several factors bear evidence of chemosynthetic ecosystem occurrence in the Brazilian coast; these motivated our investigation to sample three pockmarks located on the continentalslopeoffSE Brazil (26°S and 46°W) at ∼700 m depth. The crater-like features were ∼1 km in diameter and 100 m in depth, and were identified with an echo-sounder (EK-500). They were sampled along two transects using a rectangular dredge. Our main objective was to identify possible evidence of a seep-related community. The surrounding sediments of the pockmarks seem to be filled with coral rubble harboring a rich fauna of metazoans including epilithic and chasmolithic organisms. A total of 9565 organisms were sampled. The most abundant group was the Ophiuroidea, followed by Cirripedia and Polychaeta. A number of new occurrences and new species were registered. The polychaete worm Amelinna was the first record for the Atlantic Ocean, which has been found in reducing habitats such as wood islands. The echo-sounder records also showed the presence of big deepwatercoral mounds associated with the edge of the pockmarks. These features are ∼ 20 m in height and from 180 to 360 m wide. Records of demersal fishes were also registered right above coral mounds. The presence of deepwatercoral mounds at the edge of pockmarks may be related to the flow of the cold, oxygen-rich Antarctic Intermediate Water over the bottom, or else may benefit from the fertilization of the water by the microseepage of hydrocarbons from the sediment. We suggest a more thorough survey in order to map and recognize these environments. Furthermore, our findings may shed some light on new research perspectives concerning the ecology, biogeography and evolution of reducing habitats off the Brazilian coast.
format Article in Journal/Newspaper
author Sumida, Paulo Yukio Gomes
Yoshinaga, Marcos Yukio
Madureira, Lauro Antonio Saint Pastous
Hovland, Martin
author_facet Sumida, Paulo Yukio Gomes
Yoshinaga, Marcos Yukio
Madureira, Lauro Antonio Saint Pastous
Hovland, Martin
author_sort Sumida, Paulo Yukio Gomes
title Seabed pockmarks associated with deepwater corals off SE Brasilian continental slope, Santos Basin
title_short Seabed pockmarks associated with deepwater corals off SE Brasilian continental slope, Santos Basin
title_full Seabed pockmarks associated with deepwater corals off SE Brasilian continental slope, Santos Basin
title_fullStr Seabed pockmarks associated with deepwater corals off SE Brasilian continental slope, Santos Basin
title_full_unstemmed Seabed pockmarks associated with deepwater corals off SE Brasilian continental slope, Santos Basin
title_sort seabed pockmarks associated with deepwater corals off se brasilian continental slope, santos basin
publishDate 2004
url http://repositorio.furg.br/handle/1/3906
geographic Antarctic
geographic_facet Antarctic
genre Antarc*
Antarctic
genre_facet Antarc*
Antarctic
op_relation SUMIDA, Paulo Yukio Gomes et al. Seabed pockmarks associated with deepwater corals off SE Brasilian continental slope, Santos Basin. Marine Geology, v. 207, p. 159-167, 2004. Disponível em:<http://ac.els-cdn.com/S0025322704000726/1-s2.0-S0025322704000726-main.pdf?_tid=1afd9348408dc1d8207f207d78f93350&acdnat=1340365926_b0203db1a478ec98ab2da6af7f9a735a>. Acesso em: 22 jun. 2012.
http://repositorio.furg.br/handle/1/3906
op_rights restrict access
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