2001
DOI: 10.1016/s0031-0182(00)00216-9
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An Early Jurassic oligohaline ostracod assemblage within the marine carbonate platform sequence of the Venetian Prealps, NE Italy

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Cited by 25 publications
(23 citation statements)
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“…Valves with ''cup in cup'' structure are present in this ostracod species. This arrangement of ostracod valves has been reported on several occasions from a number of fossil sequences (Wakefield & Athersuch, 1990;Wakefield, 1995;Boomer et al, 2001;Carignano & Ballent, 2009). Fontana & Ballent (2005) documented this phenomenon in a recent cypridid from southern Buenos Aires Province, Argentina.…”
Section: Paleoecology-environment Of Depositionsupporting
confidence: 75%
“…Valves with ''cup in cup'' structure are present in this ostracod species. This arrangement of ostracod valves has been reported on several occasions from a number of fossil sequences (Wakefield & Athersuch, 1990;Wakefield, 1995;Boomer et al, 2001;Carignano & Ballent, 2009). Fontana & Ballent (2005) documented this phenomenon in a recent cypridid from southern Buenos Aires Province, Argentina.…”
Section: Paleoecology-environment Of Depositionsupporting
confidence: 75%
“…Wakefield & Athersuch, 1990;Wakefield, 1995;Boomer et al, 2001). Whatley (as mentioned in Boomer et al, 2001: 342) recorded this phenomenon in Recent ostracods in the Coorong in South Australia.…”
Section: Depositional Environment Conditionsmentioning
confidence: 93%
“…The westernmost sector (Monte Baldo and Adige River area) is mainly characterised by marginal oolitic shoals. The typical facies of the Rotzo Formation are ooidal, peloidal, bioclastic and intraclastic limestones with marly and clayey horizons rich in plant remains and thin coal levels (Broglio Loriga and Neri 1976;Boomer et al 2001;Roghi and Romano 2008;Posenato and Masetti 2012). Macrofossils are common and include molluscs (large and small bivalves such as Lithiotis s.l.…”
Section: Geological and Palaeogeographic Settingmentioning
confidence: 99%
“…Thaumatoporella parvovesiculifera) and ostracods (e.g. Phraterfabanella tridentinensis), although foraminifera are locally rare (Bosellini and Broglio Loriga 1971;Fugagnoli and Loriga Broglio 1998;Boomer et al 2001). The lower part of the Rotzo Formation yielded also a rich palynoflora including Ischyosporites variegatus (Couper) Schulz, 1967, Leptolepidites major Couper, 1953, Matonisporites crassiangulatus Levet-Carette, 1964, and Trilites lygodioides Mai, 1967, that was previously attributed to the Toarcian (Schulz 1967), but is now known to extend to the Sinemurian-Pliensbachian (Avanzini et al 2006).…”
Section: Geological and Palaeogeographic Settingmentioning
confidence: 99%