Nikolov Vladimir, Pavlishina Polina, Dochev Docho, Brusatte Stephen L
National Museum of Natural History at the Bulgarian Academy of Sciences, 1 Tsar Osvoboditel Blvd., 1000 Sofia, Bulgaria.
Department of Geology, Paleontology, and Fossil Fuels, Sofia University 'St. Kliment Ohridski', 15 Tsar Osvoboditel Blvd., 1504 Sofia, Bulgaria.
Swiss J Palaeontol. 2025;144(1):41. doi: 10.1186/s13358-025-00388-z. Epub 2025 Jul 29.
The Upper Cretaceous European vertebrate fossil record has improved significantly in the past three decades but there still remain chronostratigraphic and geographic gaps, which obscure our understanding of the paleobiogeography and evolution within the insular environments of the Late Cretaceous European Archipelago. Recently, a new vertebrate locality of late Santonian-early Campanian age was discovered in westernmost Bulgaria, promising to fill some of these gaps. Here, we use a multidisciplinary approach involving palynology, paleontology and paleohistology to investigate aspects of the paleoecology and taphonomy of this new locality and to provide preliminary information on its taxonomic contents. Palynomorph data shows that the flora was dominated by angiosperms of the Normapolles group with subordinate presence of ferns and only rare gymnosperms. The association of the pollen taxa and supports latest Santonian to early Campanian age for the vertebrate-bearing strata. The floral composition and especially a number of fern spore humidity indicators imply the existence of a generally humid subtropical climate, with some seasonal droughts. Using palynofacies analysis, we infer a coastal, proximal shelf to oxidated deltaic or lagoonal depositional environment for the examined sedimentary succession. The locality has so far yielded 250 vertebrate specimens collected from eight strata. There are at least seven clades present, including lamniform sharks, lepisosteid gars, amphibians, turtles, crocodylomorphs, ornithopod and titanosaur dinosaurs, and possibly pterosaurs. Semi-aquatic and aquatic animals dominate the assemblage. Most common are turtles (about 30% of the sample), followed by dinosaurs. Skeletal elements are disarticulated, isolated and mostly fragmentary. Fossils are not sorted by size. Many of the fossil bones show signs of abrasion and bioerosion, both micro- and macroscopically. Paleohistological data reveal that all sampled dinosaur bones belong to subadult or adult individuals. We interpret the site to be an attritional assemblage. Taxonomic comparisons with other well-known Santonian to Maastrichtian fossil assemblages from Central (Hungary and Austria) and Eastern Europe (Romania and Serbia) indicate similarities with both the Santonian Iharkút-Ajka vertebrate fauna of Hungary and the younger Haţeg Island fauna of Romania, although additional material and more precise taxonomic identification of the Bulgarian fossils is needed. Our work presents the first more in-depth look at life on land in this currently underexplored part of the Late Cretaceous European Archipelago.
The online version contains supplementary material available at 10.1186/s13358-025-00388-z.
在过去三十年里,上白垩统欧洲脊椎动物化石记录有了显著改善,但仍存在年代地层和地理上的空白,这使我们对晚白垩世欧洲群岛岛屿环境中的古生物地理学和进化的理解变得模糊。最近,在保加利亚最西部发现了一个晚桑托阶 - 早坎帕阶的新脊椎动物产地,有望填补其中一些空白。在这里,我们采用了一种多学科方法,涉及孢粉学、古生物学和古组织学,来研究这个新产地的古生态学和埋藏学方面,并提供其分类内容的初步信息。孢粉形态数据表明,植物群以诺马孢粉组的被子植物为主,蕨类植物次之,裸子植物稀少。花粉类群的组合支持含脊椎动物地层的年代为最晚桑托阶至早坎帕阶。植物组成,尤其是一些蕨类孢子湿度指标表明存在普遍潮湿的亚热带气候,伴有一些季节性干旱。通过孢粉相分析,我们推断所研究的沉积层序为海岸、近岸陆架至氧化的三角洲或泻湖沉积环境。该产地迄今已从八个地层中采集到250件脊椎动物标本。至少有七个类群,包括鼠鲨目鲨鱼、雀鳝、两栖动物、龟、鳄形类、鸟脚亚目和泰坦巨龙类恐龙,可能还有翼龙。半水生和水生动物在组合中占主导地位。最常见的是龟(约占样本的30%),其次是恐龙。骨骼元素脱节、孤立且大多破碎。化石没有按大小分类。许多化石骨骼在微观和宏观上都有磨损和生物侵蚀的迹象。古组织学数据表明,所有采样的恐龙骨骼都属于亚成体或成年个体。我们将该遗址解释为一个损耗性组合。与来自中欧(匈牙利和奥地利)和东欧(罗马尼亚和塞尔维亚)其他著名的桑托阶至马斯特里赫特阶化石组合进行分类比较表明,它与匈牙利的桑托阶伊哈尔库特 - 奥伊卡脊椎动物群和罗马尼亚较年轻的哈采格岛动物群都有相似之处,不过还需要更多的材料和对保加利亚化石进行更精确的分类鉴定。我们的工作首次更深入地审视了晚白垩世欧洲群岛这个目前未被充分探索地区的陆地生物。
在线版本包含可在10.1186/s13358 - 025 - 00388 - z获取的补充材料。