A Middle Pleistocene hippo tracksite at Gombore II-2 (Melka Kunture, Upper Awash, Ethiopia)

作者：Altamura Flavio^*; Melis Rita T; Mussi Margherita

来源：Palaeogeography, Palaeoclimatology, Palaeoecology, 2017, 470: 122-131.

DOI：10.1016/j.palaeo.2017.01.022

• Main Ethiopian Rift
• Hippopotamus amphibius
• Vertebrate ichnology
• Resilience to volcanic events

In this paper we describe exceptionally well-preserved evidence of hippo activity at Gombore 11-2, a 700,000 year-old site at Melka Kunture, at 2000 m asl in the Ethiopian highlands, in the Upper Awash Valley. We excavated and made casts of footprints that had been left after a volcanic eruption. The 3D casts provide a detailed record of the outer anatomy and soft tissues of Pleistocene hippos. They reveal for the first time the shape of the legs and feet of the animals. Gombore 11-2 also provides information on the behavior of past hippos. This prominent species of the African wildlife affects the vegetation and the landscape, and acts as a geomorphological agent. The animals wallow beside bodies of water and erode deep trails linking them to pastures. At Gombore 11-2 the trampling marks converge toward an erosional feature that we interpret as a fossil trail, documenting an early Middle Pleitocene behavior similar to that of today. Signs of trampling and erosional features interpreted as hippo trails have also been described in Pliocene and early Pleistocene levels at Olduvai and Koobi Fora. We further underline that the hippo population of this tract of the valley was resilient and reestablished itself not long time after the volcanic eruption.

• 出版日期2017-3-15