Ichnological research on Tibetan hominin hand and footprints and its indicative significance
Authors: Zhang, D.D., Bennett, M.R. et al.
Journal: Chinese Science Bulletin
Volume: 70
Issue: 10
Pages: 1329-1341
eISSN: 2095-9419
ISSN: 0023-074X
DOI: 10.1360/TB-2023-1219
Abstract:Exploration of human ichnology began in the 20th century and significant advancements have been made in the 21st century. These imprints, including footprints and handprints, are invaluable resources for elucidating the evolutionary trajectories and living contexts of ancient human populations. Unlike traditional archaeological remains, such as human fossils, cultural layers, and faunal and floral remains, exceptionally well-preserved imprints can offer unique insights into aspects like muscle morphology, mobility patterns, gender distinctions, height, and ancient population demographics. On a global scale, noteworthy ichnological research includes analyses of hominin tracks found in volcanic ash in Tanzania, Africa (dated to ~3.66 Ma), footprints at White Sands National Park in New Mexico, USA (dated to 23–20 ka), and handprints discovered in Indonesian caves (dated to 51.8 ka). These imprints have significantly contributed to research on the evolution, migration, and behavioral cognition of ancient human societies. However, relatively little attention has been paid to the study of ancient human ichnology within China, and international investigations of imprints within travertine deposits are scarce. Since the 1980s, over 100 archaic human handprints and footprints have been discovered at different elevations within the multilayered sediments of the Quesang hot spring travertine, in the central Tibetan Plateau. This travertine is composed of calcium carbonate formed from the precipitation of CaCO
Source: Scopus
Ichnological research on Tibetan hominin hand and footprints and its indicative significance
Authors: Zhang, D., Bennett, M.R. et al.
Journal: CHINESE SCIENCE BULLETIN-CHINESE
Volume: 70
Issue: 10
Pages: 1329-1341
eISSN: 2095-9419
ISSN: 0023-074X
DOI: 10.1360/TB-2023-1219
Source: Web of Science (Lite)