Aguilera Orangel, Luz Zoneibe, Carrillo-Briceño Jorge D, Kocsis László, Vennemann Torsten W, de Toledo Peter Mann, Nogueira Afonso, Amorim Kamilla Borges, Moraes-Santos Heloísa, Polck Marcia Reis, Ruivo Maria de Lourdes, Linhares Ana Paula, Monteiro-Neto Cassiano
Departamento de Biologia Marinha, Instituto de Biologia, Universidade Federal Fluminense, Niterói, Rio de Janeiro, Brasil.
Instituto de Geociências, Universidade Federal do Pará, Belém, Pará, Brasil.
PLoS One. 2017 Aug 23;12(8):e0182740. doi: 10.1371/journal.pone.0182740. eCollection 2017.
The lower Miocene Pirabas Formation in the North of Brazil was deposited under influence of the proto-Amazon River and is characterized by large changes in the ecological niches from the early Miocene onwards. To evaluate these ecological changes, the elasmobranch fauna of the fully marine, carbonate-rich beds was investigated. A diverse fauna with 24 taxa of sharks and rays was identified with the dominant groups being carcharhiniforms and myliobatiforms. This faunal composition is similar to other early Miocene assemblages from the proto-Carribbean bioprovince. However, the Pirabas Formation has unique features compared to the other localities; being the only Neogene fossil fish assemblage described from the Atlantic coast of Tropical Americas. Phosphate oxygen isotope composition of elasmobranch teeth served as proxies for paleotemperatures and paleoecology. The data are compatible with a predominantly tropical marine setting with recognized inshore and offshore habitats with some probable depth preferences (e.g., Aetomylaeus groups). Paleohabitat of taxa particularly found in the Neogene of the Americas (†Carcharhinus ackermannii, †Aetomylaeus cubensis) are estimated to have been principally coastal and shallow waters. Larger variation among the few analyzed modern selachians reflects a larger range for the isotopic composition of recent seawater compared to the early Miocene. This probably links to an increased influence of the Amazon River in the coastal regions during the Holocene.
巴西北部的中新世早期皮拉巴斯组是在原亚马逊河的影响下沉积形成的,其特点是从中新世早期开始生态位发生了巨大变化。为了评估这些生态变化,对完全海洋环境、富含碳酸盐的地层中的板鳃类动物群进行了研究。已识别出一个多样化的动物群,包括24种鲨鱼和鳐鱼分类单元,其中占主导地位的类群是真鲨形目和鲼形目。这种动物群组成与原加勒比生物省的其他中新世早期组合相似。然而,与其他地区相比,皮拉巴斯组具有独特的特征;它是热带美洲大西洋海岸描述的唯一新近纪化石鱼类组合。板鳃类牙齿的磷酸盐氧同位素组成被用作古温度和古生态的代理指标。这些数据与一个主要为热带海洋环境相符合,其中存在公认的近岸和离岸栖息地,并且一些类群可能有特定的深度偏好(例如,前口鲼属类群)。特别是在美洲新近纪发现的分类单元(†阿克曼氏真鲨、†古巴前口鲼)的古栖息地估计主要是沿海和浅水环境。与中新世早期相比,少数分析的现代板鳃类动物之间较大的差异反映了近期海水同位素组成的更大范围。这可能与全新世期间亚马逊河对沿海地区的影响增加有关。