2020
DOI: 10.1590/0001-3765202020191096
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Influence of depth on bryozoan richness and distribution from the continental shelf of the northern coast of Bahia State, north-eastern Brazil

Abstract: Biological and abiotic processes infl uence ecosystem structure and species distribution. For bryozoan assemblages, depth, substratum and habitat structure are among the main factors infl uencing their distribution. Ecological studies on bryozoan fauna from Brazil are scarce and factors affecting the distribution and/or diversity of this common group are obscure. Here we attempted to verify the infl uence of bathymetry on bryozoan richness on the north shore of Bahia State, northeastern Brazil. We identifi ed … Show more

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Cited by 6 publications
(3 citation statements)
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“…During the Mesoneoproterozoic PanAfrican-Brazilian orogenic events (HEILBRON et al, 2000), the São Francisco Craton was part of the greater Late Upper Proterozoic São Francisco-Congo-Kalahari craton (HASUI, 2010), which is a Gondwanide continental block that originally extended east into South Africa and south into Antarctica (HASUI, 2010). With the Mesozoic break up (TROMPETTE et al, 1992), South America and Africa drifted apart in the Valanginian (LARSON; LADD, 1973; SIEDNER; MITCHEL, 1976), probably because of Cretaceous hot spots (ULBRICH; GOMES, 1981; THOMAZ FILHO; RODRIGUES, 1999; WHITE; MCKENZIE, 1989), which led to doming, uplift, as well as rifting processes and ultimately caused continental fragmentation (ALMEIDA 1976; SIEDNER; MITCHELL, 1976; COX, 1989).…”
Section: Introductionmentioning
confidence: 99%
“…During the Mesoneoproterozoic PanAfrican-Brazilian orogenic events (HEILBRON et al, 2000), the São Francisco Craton was part of the greater Late Upper Proterozoic São Francisco-Congo-Kalahari craton (HASUI, 2010), which is a Gondwanide continental block that originally extended east into South Africa and south into Antarctica (HASUI, 2010). With the Mesozoic break up (TROMPETTE et al, 1992), South America and Africa drifted apart in the Valanginian (LARSON; LADD, 1973; SIEDNER; MITCHEL, 1976), probably because of Cretaceous hot spots (ULBRICH; GOMES, 1981; THOMAZ FILHO; RODRIGUES, 1999; WHITE; MCKENZIE, 1989), which led to doming, uplift, as well as rifting processes and ultimately caused continental fragmentation (ALMEIDA 1976; SIEDNER; MITCHELL, 1976; COX, 1989).…”
Section: Introductionmentioning
confidence: 99%
“…These interdependencies within river ecosystems ensure that alterations in one constituent reverberate throughout the food chain, affecting organisms at various trophic levels. Specifically, regarding PKD, bryozoan colonies, as living animals, are equally sensitive to habitat composition changes and water modifications [33][34][35].…”
Section: Introductionmentioning
confidence: 99%
“…A área de estudo está inserida na Bacia de Santos e segundo Almeida (1976) é uma depressão meso-cenozóica, tectônica repleta de basaltos e sedimentos, localizada na margem continental entre o estado do Rio de Janeiro e Santa Catarina.…”
Section: áRea De Estudounclassified