Sahara's surface transformation forced an abrupt hydroclimate decline and Neolithic culture transition in northern China.

ABSTRACT: The remote forcing from land surface changes in the Sahara is hypothesized to play a pivotal role in modulating the intensity of the East Asian summer monsoon (EASM) through ocean-atmospheric teleconnections. This modulation has far-reaching consequences, particularly in facilitating societal shifts documented in northern China. Here, we present a well-dated lake-level record from the Daihai Lake Basin in northern China, providing quantitative assessments of Holocene monsoonal precipitation and the consequent migrations of the northern boundary of the EASM. Our reconstruction, informed by a water-and-energy balance model, indicates that annual precipitation reached ∼700 mm during 8-5 ka, followed by a rapid decline to ∼550 mm between 5 and 4 ka. This shift coherently aligns with a signific

SUBMITTER: Hou Y 

PROVIDER: S-EPMC10777076 | biostudies-literature | 2024 Jan

REPOSITORIES: biostudies-literature