2012
DOI: 10.1016/j.annpal.2012.02.001
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The decapod community from the Early Pliocene (Zanclean) of “La Serra” quarry (San Miniato, Pisa, Toscana, central Italy): sedimentology, systematics, and palaeoenvironmental implications

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Cited by 20 publications
(14 citation statements)
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“…Even though incomplete, we ascribe confidently to this species three propodi for the abovementioned characters, sharing with the propodus of the extant Pisa armata . This species was already reported in the fossil record of Italy from the Early Pliocene of “La Serra” quarry (Pisa, Tuscany, central Italy) (Garassino et al , 2012), and from the Late Pleistocene of Monte Pellegrino (Palermo, Sicily, southern Italy) (Gemmellaro, 1914). In the Mediterranean Sea, P. armata occupies usually rocky hard grounds or mud-sandy rich in weeds, ranging from 1 to 500 meter deep, but commonly between 50-160 meter deep (Falciai & Minervini, 1992).…”
Section: Discussionmentioning
confidence: 58%
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“…Even though incomplete, we ascribe confidently to this species three propodi for the abovementioned characters, sharing with the propodus of the extant Pisa armata . This species was already reported in the fossil record of Italy from the Early Pliocene of “La Serra” quarry (Pisa, Tuscany, central Italy) (Garassino et al , 2012), and from the Late Pleistocene of Monte Pellegrino (Palermo, Sicily, southern Italy) (Gemmellaro, 1914). In the Mediterranean Sea, P. armata occupies usually rocky hard grounds or mud-sandy rich in weeds, ranging from 1 to 500 meter deep, but commonly between 50-160 meter deep (Falciai & Minervini, 1992).…”
Section: Discussionmentioning
confidence: 58%
“…We ascribe the studied specimens to the extant I. nucleus , because it shares the same above-mentioned morphological characters. A review of the morphological characters of this species carried on by Garassino and Pasini (2012), pointed out that all the specimens previously reported from the Pliocene of Italy and erroneously ascribed to I. pliocaenica Ristori, 1891, should be instead ascribed to I. nucleus (for discussion see Garassino et al, 2010a, 2012, 27-30; Garassino & Pasini, 2012, 43-46). Moreover I. nucleus , was recently reported from the Early Pleistocene (Emilian) of Pomezia (Roma, Lazio, central Italy) (Garassino et al , 2010a; Garassino & Pasini, 2012), and from the Zanclean (Early Pliocene) of “La Serra” quarry (Pisa, Tuscany, central Italy) by Garassino et al .…”
Section: Discussionmentioning
confidence: 99%
“…Deep‐water decapod crustacean assemblages from the Neogene fossil record are sparse (Hyžný and Schlögl and references therein), although recently several reports from the Pliocene and Pleistocene of Italy were published (Garassino et al . ; Baldanza et al . ; Pasini et al .…”
Section: Discussionmentioning
confidence: 99%
“…The specimens differ from Goneplax rhomboides (Linnaeus, ) (Garassino et al . ), in having more convex anterolateral margins with shorter anterolateral teeth. Relatively wide front is reminiscent of published figure of Goneplax sacci Crema, ; the species was recently considered a nomen dubium by Garassino et al .…”
Section: Systematic Palaeontologymentioning
confidence: 99%
“…Asseveral criticisms were pointed out, and as they emerged also in other case studies [45,70,71,97], a critical review of data would be expected.…”
Section: Proposed Stratigraphic Scheme For Western Umbriamentioning
confidence: 94%