2020
DOI: 10.1016/j.jsames.2020.102795
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First evidence of fossil snapping shrimps (Alpheidae) in the Neotropical region, with a checklist of the fossil caridean shrimps from the Cenozoic

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Cited by 7 publications
(3 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%
“…have been recorded in France and Austria (Mü ller, 1998;Cluzaud et al, 2014;Jagtet et al, 2015). Recently, Lima et al (2020) also recorded the first neotropical evidence of early and middle Miocene alpheids based on claw fingertips from the Pirabas Formation (Fm), Brazil. The early-middle Miocene (Burdigalian-Serravallian) records of alpheids (based only on claw fingertips) are quite common in different parts of Europe, viz., Austria, The Netherlands, Czech Republic, Poland, and Slovakia, with only a single fossil record, to date, from the upper Miocene (Tortonian) of France (Hyžný et al, 2017;Fig.…”
mentioning
confidence: 99%