2006
DOI: 10.25249/0375-7536.2006364648650
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Primeiro Registro De Fósseis De Aves Marinhas Na Planície Costeira Do Rio Grande Do Sul, Brasil

Abstract: Resumo Este trabalho apresenta a ocorrência inédita de fósseis de aves marinhas procedentes de depósitos fossilíferos pleistocênicos submersos ao longo da plataforma continental interna do estado do Rio Grande do Sul. Os fósseis apresentados foram coletados em trabalhos de campo realizados entre os anos de 1999 e 2003 e consistem de três vértebras cervicais e parte de um tibiotarso esquerdo. A morfologia e tamanho desses fósseis são semelhantes às de uma ave marinha procelariforme da espécie Thalassarche melan… Show more

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Cited by 8 publications
(6 citation statements)
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“…This process seems to be the main one responsible for the low proportion of large cranial and postcranial remains of large-bodied taxa such as sloths, toxodontids and gomphotheriids. While smaller, more compact remains of small-bodied taxa are easily transported by waves under normal conditions, the larger elements can be transported only by high energy waves, which occur only during extreme storms (Calliari et al, 1998;Lopes et al, 2006). Thus, these large remains rarely come to the beach, but once deposited there, would be removed only by a similar storm, so their residence time on the beach is longer than that of a small fossil continuously moved by normal wave regimes.…”
Section: Discussionmentioning
confidence: 99%
See 1 more Smart Citation
“…This process seems to be the main one responsible for the low proportion of large cranial and postcranial remains of large-bodied taxa such as sloths, toxodontids and gomphotheriids. While smaller, more compact remains of small-bodied taxa are easily transported by waves under normal conditions, the larger elements can be transported only by high energy waves, which occur only during extreme storms (Calliari et al, 1998;Lopes et al, 2006). Thus, these large remains rarely come to the beach, but once deposited there, would be removed only by a similar storm, so their residence time on the beach is longer than that of a small fossil continuously moved by normal wave regimes.…”
Section: Discussionmentioning
confidence: 99%
“…During autumn and winter, storm waves erode these concentrations and transport the fossils to the beach, where they are collected. Besides terrestrial mammals, the concentrations also contain remains of marine mollusks , corals, echinoderms, crustaceans (Buchmann, 1994;Lopes, 2011), teleost (Richter, 1987) and elasmobranch fishes (Buchmann & Rincón Filho, 1997), pinnipeds (Oliveira & Drehmer, 1997), cetaceans (Cunha, 1982;Ribeiro et al, 1998), seabirds (Lopes et al, 2006) and reptiles (Hsiou & Fortier, 2007;Hsiou, 2009).…”
Section: Introductionmentioning
confidence: 99%
“…Although remains of several marine organisms such as teleost and elasmobranch fishes (Richter, 1987;Buchmann and Rincón Filho, 1997), shellfish (Figueiredo (1975); , echinoderms, crustaceans (Buchmann, 1994;Lopes, 2009), pinnipeds (Oliveira and Drehmer, 1997), cetaceans (Cunha, 1982;Ribeiro et al, 1998) and seabirds (Lopes et al, 2006) are found in these concentrations, the most remarkable are the fossils of terrestrial mammals (Fig. 2).…”
Section: Fossils From the Inner Continental Shelfmentioning
confidence: 97%
“…These fossils are rolled and collected at the beach, being similar to those from Arroio Chuí, and associated to marine fossils (Ribeiro et al, 1998). They present dark coloration, high density and carbonate cement, suggesting reworking by the marine ambient (Lopes et al, 2001). After the deposition in lagoonal ambient (probably the Lagoon III), posterior to the fossilization process, they were reworked and cemented by calcium carbonate in a marine shore environment and preserved in sandstones and carbonate in the parcels and submerged banks (foreshore and continental platform).…”
Section: P R O V a Smentioning
confidence: 99%