First vertebrate faunal record from submerged Sundaland: The late Middle Pleistocene, hominin-bearing fauna of the Madura Strait

H.W.K. Berghuis , Gert van den Bergh , Thijs van Kolfschoten , Unggul Prasetyo Wibowo , Iwan Kurniawan , Shinatria Adhityatama , Indra Sutisna , Ivo Verheijen , Eduard Pop , A. Veldkamp , Josephine C.A. Joordens
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Abstract

The Sunda Shelf currently holds the world’s largest shelf sea. During Pleistocene sea-level lowstands the area emerged, forming a vast landmass called Sundaland. Intermittently exposed Sundaland played an important role in the regional vertebrate biogeography and evolution of species including Homo erectus and, in the Late Pleistocene, Homo sapiens. So far, our models of the Pleistocene biogeography of Sundaland were based on the distribution of extant species and on island fossil assemblages, notably from Java (Indonesia). Here we present the first vertebrate fossil record from subsea Sundaland. The fossils derive from the sandy fill of a lowstand valley of the Solo River in the Madura Strait, which was OSL-dated to 162 ± 31 and 119 ± 27 ka. The cemented sand was recently extracted and used for a landfill in the port of Surabaya. The assemblage consists of at least 36 species and provides a unique insight into the lowland fauna of emerged Sundaland, during the late Middle Pleistocene. The lowland river had a rich reptile community, consisting of various turtle species, crocodilians, varanids, and pythons. The nearby estuary was frequented by several shark species, including the extinct Hemipristis serra, as well as several species of stingrays. Some of these also ascended the river. The lowland plains surrounding the river were populated by herbivores such as Hippopotamidae and several species of Bovidae, Cervidae, and Proboscidea. The terrestrial community represents a grass-dominated environment and is similar to the contemporaneous fossil assemblage of Ngandong (Java). However, on a detailed level, there are conspicuous differences. For example, Duboisia santeng, Axis lydekkeri, and Epileptobos groeneveldtii are absent in Ngandong and were generally believed to have become extinct by the end of the Middle Pleistocene. Their presence in the Madura Strait assemblage shows that the species persisted on the lowland plains. Interesting is also the presence of more rarely encountered species such as Varanus komodoensis, Macaca sp. and Homo erectus on the lowland plains. Metrically, Elephas sp. molars from the Madura Strait site are relatively high-crowned, whereas Bos palaeosondaicus is relatively small-statured compared to its Middle Pleistocene relatives from Java. The fossil fauna from the Madura Strait reflects a thus far unknown vertebrate coastal lowland community that lived in and around the lower reaches of the Middle Pleistocene Solo River.
首个来自水下巽他兰的脊椎动物区系记录:中更新世晚期,马都拉海峡有人族的动物群
巽他大陆架目前拥有世界上最大的大陆架海。在更新世海平面低潮时期,该地区出现,形成了一个巨大的陆地,称为Sundaland。间断性暴露的Sundaland在区域脊椎动物生物地理和物种进化中发挥了重要作用,包括直立人,以及晚更新世的智人。到目前为止,我们的Sundaland更新世生物地理模型是基于现存物种的分布和岛屿化石组合,特别是来自印度尼西亚爪哇的化石组合。在这里,我们展示了来自海底Sundaland的第一个脊椎动物化石记录。这些化石来自于马都拉海峡梭罗河低洼河谷的沙质填埋物,岩石年代分别为162 ± 31和119 ± 27 ka。这些胶结的沙子最近被提取出来,用于泗水港的一个垃圾填埋场。该组合由至少36个物种组成,为中更新世晚期出现的巽他兰低地动物群提供了独特的见解。这条低地河流有丰富的爬行动物群落,包括各种乌龟、鳄鱼、变形兽和蟒蛇。附近的河口经常有几种鲨鱼出没,包括已灭绝的半角鲨,以及几种黄貂鱼。其中一些人也上了河。河流周围的低地平原上栖息着食草动物,如河马科和一些牛科、鹿科和喙科动物。陆生群落表现为以草为主的环境,与爪哇地区Ngandong的同时期化石组合相似。然而,在细节层面上,有明显的差异。例如,Duboisia santeng、Axis lydekkeri和Epileptobos groeneveldtii在广东没有发现,一般认为它们在中更新世末期已经灭绝。它们在马杜拉海峡的存在表明该物种在低地平原上持续存在。有趣的是,在低地平原上还发现了一些罕见的物种,如瓦拉努斯·科莫多人、马卡人和直立人。从度量上来说,来自马杜拉海峡遗址的大象sp.臼齿的冠相对较高,而与爪哇的中更新世近亲相比,bospalaeosondaicus的体型相对较小。来自马杜拉海峡的化石动物群反映了一个迄今为止未知的脊椎动物沿海低地群落,它生活在中更新世梭罗河下游及其周围。
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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