Nuevos registros de Otodontidae Glickman 1964B (Chondrichthyes) para el sur de la Península de Nicoya, Puntarenas, Costa Rica

César A. Laurito, A. Valerio, Cristian Calvo
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Abstract

The Otodus genus and its species have been recorded in Southern Central America since the Eocene epoch, its remains are associated with calcareous or clastic sediments typical of sublitoral or inner neritic environments. One of these geological formations is Santa Teresa Fm. with a Middle Miocene to Lower Pliocene age range, outcropping in the Pacific margin and the elevated parts at the southern end of the Nicoya Peninsula, where a series of finds of Otodus (Megaselachus) chubutensis and Otodus (Megaselachus) megalodon had been previously reported. Over several decades, dental remains associated with Otodus genus have been recorded at Southern Nicoya Peninsula, fortuitous finds, some of them without direct geological context. However, the locations given by the people who made the findings, allow us to establish with some degree of certainty the sedimentary units from which the samples came, allowing us to increase the knowledge of the abundance and diversity of the fossil record of these giant sharks.
哥斯达黎加蓬塔雷纳斯尼科亚半岛南部耳齿鱼科Glickman 1964B (Chondrichthyes)的新记录
Otodus属及其种自始新世以来就在中美洲南部有记录,其遗迹与典型的亚浅海或内浅海环境的钙质或碎屑沉积物有关。其中一个地质构造是圣特蕾莎Fm。在太平洋边缘和尼科亚半岛南端的高地地区,曾发现过一系列的巨齿鲨和巨齿鲨,年龄范围为中新世中期至上新世下部。几十年来,在南尼科亚半岛,偶然发现了与耳蟾属有关的牙齿遗骸,其中一些没有直接的地质背景。然而,这些发现的人给出的地点,让我们在一定程度上确定了样本来自的沉积单元,让我们增加了对这些巨型鲨鱼化石记录的丰富性和多样性的了解。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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