Nobile Francesco, Lambert Olivier, Bianucci Giovanni, Amson Eli, Bosselaers Mark, Bosio Giulia, Pellegrino Luca, Malinverno Elisa, Di Celma Claudio, Urbina Mario, Collareta Alberto
Dipartimento di Scienze della Terra, University of Pisa, 56126 Pisa, Italy.
D.O. Terre et Histoire de La Vie, Institut Royal Des Sciences Naturelles de Belgique, 1000 Brussels, Belgium.
Life (Basel). 2025 Mar 13;15(3):452. doi: 10.3390/life15030452.
The evolution of baleen whales (Mysticeti) comprises two main phases, namely, (i) a Paleogene phase, which saw the diversification of stem lineages, and (ii) a Neogene phase, dominated by modern-looking, toothless, baleen-bearing forms in the monophyletic group Chaeomysticeti. These two phases are separated by a global turnover event coinciding with a gap-or "dark age"-in the mysticete fossil record. This dark age occurred between 23 and ~18 Ma and is apparently detected worldwide, except in Zealandia. Here, we report on a new mysticete fossil from the Lower Miocene (Burdigalian: ~19.2 Ma) strata of the Chilcatay Formation cropping out at the newly discovered locality of Cerro Tiza (East Pisco Basin, Peru), which represents a limited but precious testament from the last phase of the baleen whale dark age. Two previously mentioned, slightly geologically younger fossils from the same formation are also reappraised herein, revealing the occurrence of at least another baleen whale taxon in the upper Chilcatay strata-one that belongs in the mysticete crown group. Although the Early Miocene remains a problematic time interval for the fossil record of baleen whales, our new results encourage the search for mysticete fossils in the Lower Miocene strata of the East Pisco Basin, whose basin fill preserves a cornucopia of extraordinarily informative marine vertebrate fossils of the Cenozoic age, as well as in coeval deposits worldwide.
须鲸(Mysticeti)的演化包括两个主要阶段,即:(i)古近纪阶段,该阶段见证了干群的多样化;以及(ii)新近纪阶段,由单系类群新须鲸科(Chaeomysticeti)中形态现代、无牙且有须的形态主导。这两个阶段被一次全球更替事件分隔开来,该事件与须鲸化石记录中的一个间断期或“黑暗时代”相吻合。这个黑暗时代发生在2300万年前至约1800万年前之间,除了在西兰迪亚外,在全球范围内显然都能检测到。在此,我们报告了一种新的须鲸化石,它来自于新发现产地塞罗蒂萨(秘鲁东皮斯科盆地)出露的奇尔卡泰组(Chilcatay Formation)下中新统(布尔迪加尔阶:约1920万年前)地层,这是须鲸黑暗时代最后阶段的一份有限但珍贵的见证。本文还重新评估了来自同一地层、地质年代稍晚的另外两种化石,揭示了奇尔卡泰组上部地层中至少还有另一个须鲸分类单元的存在——一个属于须鲸冠群的分类单元。尽管早中新世对于须鲸化石记录来说仍然是一个存在问题的时间间隔,但我们的新结果鼓励在东皮斯科盆地的下中新统地层中寻找须鲸化石,该盆地的沉积物中保存了大量丰富的、极具信息价值的新生代海洋脊椎动物化石,同时也鼓励在全球同期沉积物中寻找须鲸化石。