Subtropical Convergence Environments 1997
DOI: 10.1007/978-3-642-60467-6_4
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Environment and Biota of the Patos Lagoon Estuary

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Cited by 9 publications
(9 citation statements)
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“…In that study, O. argentinensis emerged as the most recently derived marine species of the genus, having as ancestor a group of freshwater species that diversified during the Pleistocene. The presumed Pleistocene age of O. argentinensis is also consistent with the geological history of formation of estuarine environments in southern Brazil (Calliari 1997) and with its close evolutionary association with the recently radiated O. perugiae complex (details in Beheregaray et al. 2002).…”
Section: Discussionsupporting
confidence: 78%
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“…In that study, O. argentinensis emerged as the most recently derived marine species of the genus, having as ancestor a group of freshwater species that diversified during the Pleistocene. The presumed Pleistocene age of O. argentinensis is also consistent with the geological history of formation of estuarine environments in southern Brazil (Calliari 1997) and with its close evolutionary association with the recently radiated O. perugiae complex (details in Beheregaray et al. 2002).…”
Section: Discussionsupporting
confidence: 78%
“…Custódia), possibly because they were colonized much more recently. For instance, estuarine conditions in Patos Lagoon date from the Pleistocene (Calliari 1997), whereas Custódia Lagoon was formed as a result of a regressive episode that followed the marine transgression of 5000 years ago (Villwock et al . 1986).…”
Section: Discussionmentioning
confidence: 99%
“…During the following prolonged regression, lasting between 60 000 and 17 000 years, the northern area evolved as a group of isolated freshwater lakes not reached by subsequent marine transgressions (Schwarzbold & Schäeffer 1984;Villwock & Tomazelli 1995). By contrast, the southern Patos-Mirim is geomorphologically classified as a partially closed lagoon (Calliari 1997). For instance, sedimentary structures and radiocarbon dating of marine fossils revealed the presence of estuarine conditions in Mirim Lake in periods as recent as 4900-4300 ya (Buchmann et al 1998).…”
Section: Discussionmentioning
confidence: 99%
“…The last significant marine transgression (maximum peak around 5000 ya) was followed by two regressive movements that formed barrier IV, the most recent barrier system of the CPRS (Villwock et al 1986). This barrier, composed of beach ridges and adjacent dunes, moulded the modern Patos Lagoon estuary (Calliari 1997) and created stable freshwater environments in Mirim Lake by isolating it from the sea (Villwock et al 1986). In the outer edge of the northern CPRS, two elongated groups of interconnected lakes were formed in the gap between barriers III and IV (Schwarzbold & Schäeffer 1984;Villwock et al 1986) Furthermore, especially for southern species, most mtDNA haplotypes seem to have originated in a very recent past: they are rare, lie in the periphery of the network, and are connected independently to the most common ones via short branches (Avise 2000).…”
Section: Discussionmentioning
confidence: 99%
“…1). The estuarine area covers the southern part of the Patos Lagoon, where a single channel links the lagoon to the South Atlantic Ocean (Garcia 1997).…”
Section: The Patos Lagoon Estuarymentioning
confidence: 99%