Aguilera Orangel, Silva Guilherme Oliveira Andrade, Lopes Ricardo Tadeu, Machado Alessandra Silveira, Dos Santos Thaís Maria, Marques Gabriela, Bertucci Thayse, Aguiar Thayanne, Carrillo-Briceño Jorge, Rodriguez Felix, Jaramillo Carlos
Universidade Federal Fluminense (UFF), Instituto de Biologia, Departamento de Biologia Marinha, e Programa de Pós-graduação em Biologia Marinha e Ambientes Costeiros, Niterói, RJ, Brasil.
Nuclear Instrumentation Laboratory, Nuclear Engineering Program/COPPE. Federal Univertsity of Rio de Janeiro (UFRJ), Rio de Janeiro, Brazil.
PLoS One. 2017 Jul 26;12(7):e0181670. doi: 10.1371/journal.pone.0181670. eCollection 2017.
Fossil Diodontidae in Tropical America consist mostly of isolated and fused beak-like jawbones, and tooth plate batteries. These durophagous fishes are powerful shell-crushing predators on shallow water invertebrate faunas from Neogene tropical carbonate bottom, rocky reefs and surrounding flats. We use an ontogenetic series of high-resolution micro CT of fossil and extant species to recognize external and internal morphologic characters of jaws and tooth plate batteries. We compare similar sizes of jaws and/or tooth-plates from both extant and extinct species. Here, we describe three new fossil species including †Chilomycterus exspectatus n. sp. and †Chilomycterus tyleri n. sp. from the late Miocene Gatun Formation in Panama, and †Diodon serratus n. sp. from the middle Miocene Socorro Formation in Venezuela. Fossil Diodontidae review included specimens from the Neogene Basins of the Proto-Caribbean (Brazil: Pirabas Formation; Colombia: Jimol Formation, Panama: Gatun and Tuira formations; Venezuela: Socorro and Cantaure formations). Diodon is present in both the Atlantic and Pacific oceans, whereas the distribution of Chilomycterus is highly asymmetrical with only one species in the Pacific. It seems that Diodon was as abundant in the Caribbean/Western Atlantic during the Miocene as it is there today. We analyze the paleogeographic distribution of the porcupinefishes group in Tropical America, after the complete exhumation of the Panamanian isthmus during the Pliocene.
热带美洲的化石翻车鲀科主要由孤立的、融合的喙状颌骨以及齿板组构成。这些食硬壳动物是新近纪热带碳酸盐海底、岩礁及周边浅滩浅水无脊椎动物群的强大贝壳碾碎型捕食者。我们利用化石和现存物种的高分辨率微型计算机断层扫描个体发育系列来识别颌骨和齿板组的外部和内部形态特征。我们比较现存和已灭绝物种相似大小的颌骨和/或齿板。在此,我们描述了三个新的化石物种,包括来自巴拿马晚中新世加通组的†期待刺鲀新种和†泰勒刺鲀新种,以及来自委内瑞拉中新世中期索科罗组的†锯齿鲀新种。翻车鲀科化石综述涵盖了原加勒比地区新近纪盆地的标本(巴西:皮拉巴斯组;哥伦比亚:希莫尔组;巴拿马:加通组和图伊拉组;委内瑞拉:索科罗组和坎陶雷组)。翻车鲀属在大西洋和太平洋均有分布,而刺鲀属的分布极不对称,在太平洋仅有一个物种。在新近纪期间,翻车鲀属在加勒比海/西大西洋似乎与如今一样丰富。我们分析了上新世巴拿马地峡完全露出后热带美洲豪猪鱼群的古地理分布。