2020
DOI: 10.1016/j.jsames.2020.102517
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Uca maracoani (Crustacea, Decapoda, Ocypodidae) from a Miocene paleomangrove in Brazil: A case of evolutionary stasis among tropical American fiddler crabs

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Cited by 17 publications
(8 citation statements)
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“…The Pirabas Formation (Maury, 1925), which is of early Miocene, Aquitanian to early Burdigalian, N4 to N5 to middle Miocene, Langhian N8-N9 plankton foraminiferal biozones (Blow, 1969) (Aguilera et al, 2020a, b and references therein), consists of carbonate to mixed siliciclastic-carbonate deposits associated to shallow-water coastal settings (grainstone and consolidated packstone, stratified wackestone to packstone, and laminated mudstone) (Rossetti et al, 2013 and references therein). In addition, littoral facies (shoreface/foreshore), marginal lagoons, restricted platform environments (gray to olive mudstone and conglomeratic sandstone), and mangrove estuarine lagoons (dark mudstone, massive or laminated) have been recorded (Lima et al, 2020a, b). A diverse fossil fauna that is rich in microfossils (foraminifera, ostracodes) and macrofossils (mollusks, bryozoans, corals, echinoderms, decapods, fishes, cetaceans, and sirenids has been described (Aguilera et al, 2020a, b; Lima et al, 2020a, b).…”
Section: Geological Settingmentioning
confidence: 99%
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“…The Pirabas Formation (Maury, 1925), which is of early Miocene, Aquitanian to early Burdigalian, N4 to N5 to middle Miocene, Langhian N8-N9 plankton foraminiferal biozones (Blow, 1969) (Aguilera et al, 2020a, b and references therein), consists of carbonate to mixed siliciclastic-carbonate deposits associated to shallow-water coastal settings (grainstone and consolidated packstone, stratified wackestone to packstone, and laminated mudstone) (Rossetti et al, 2013 and references therein). In addition, littoral facies (shoreface/foreshore), marginal lagoons, restricted platform environments (gray to olive mudstone and conglomeratic sandstone), and mangrove estuarine lagoons (dark mudstone, massive or laminated) have been recorded (Lima et al, 2020a, b). A diverse fossil fauna that is rich in microfossils (foraminifera, ostracodes) and macrofossils (mollusks, bryozoans, corals, echinoderms, decapods, fishes, cetaceans, and sirenids has been described (Aguilera et al, 2020a, b; Lima et al, 2020a, b).…”
Section: Geological Settingmentioning
confidence: 99%
“…In addition, littoral facies (shoreface/foreshore), marginal lagoons, restricted platform environments (gray to olive mudstone and conglomeratic sandstone), and mangrove estuarine lagoons (dark mudstone, massive or laminated) have been recorded (Lima et al, 2020a, b). A diverse fossil fauna that is rich in microfossils (foraminifera, ostracodes) and macrofossils (mollusks, bryozoans, corals, echinoderms, decapods, fishes, cetaceans, and sirenids has been described (Aguilera et al, 2020a, b; Lima et al, 2020a, b). The specimen of Willinachoides santanai n. gen. n. sp.…”
Section: Geological Settingmentioning
confidence: 99%
“…Discussion. The fossil record of fiddler crabs is sparse and fragmentary, with only half a dozen species recognized from fossilized carapaces (e.g., Artal, 2008;Domínguez Alonso, 2008;de Gibert et al, 2013;Luque et al, 2017;Luque et al, 2018;Lima et al, 2020). Aside Afruca miocenina, the only other Miocene fiddler crab known is Uca maracoani (Latreille, 1802) from Brazil (Brito, 1972;Luque et al, 2017;Luque et al, 2018;Lima et al, 2020).…”
Section: Age Justificationmentioning
confidence: 99%
“…1). The Pirabas Formation is representative of a variety of shallow water paleoenvironments, including surf zones, tidal flats, coastal lagoons, and tidal inlet environments (Góes et al, 1990;Rossetti & Góes, 2004;Rossetti et al, 2013;Borges, 2016;Aguilera et al, 2020;Lima et al, 2020). The Pirabas Formation has been divided into two groups (α, β) and three main facies (α1, α2, and β) (Aguilera et al, 2022).…”
Section: Geological Settingmentioning
confidence: 99%