The Mediterranean region and the Levant have returned some of the clearest evidence of a
climatically dry period occurring around 4200 years ago. However, some regional evidence …

The climatic event between 4.2 and 3.9 ka BP known as the “4.2 ka event” is commonly
considered to be a synchronous global drought that happened as one pulse. However …

The Holocene is probably the most intensively studied series/epoch within the geological
record, and embodies a wide array of geomorphological, climatic, biotic and archaeological …

Gerard C. Bond established a Holocene series of North Atlantic ice-rafted debris events
based on quartz and haematite-stained grains recovered from subpolar North Atlantic …

It is well-known that the Holocene exhibits a millennial-scale climate variability. However, its
periodicity, spatio-temporal patterns and underlying processes are not fully deciphered yet …

Core-scanning X-ray Fluorescence (XRF-CS) is a well-established technique for rapid (< 30
s/interval) analysis of sediment core geochemistry at sub-mm resolution with substantially …

Identification of Holocene climate events, their temporal and spatial characteristics, and their
causal mechanisms are important for understanding past climate systems with implications …

New zoogeomorphological features discovered in dryland landscapes of Northern Africa
reflect human-animal agency since prehistory, and attest to complex, networked activities …

Despite the multiple impacts of mineral aerosols on global and regional climate and the
primary climatic control on atmospheric dust fluxes, dust-climate feedbacks remain poorly …

This study investigates the paleoenvironmental changes and fluvial dynamics in the
Inaouène River Valley of central northern Morocco over the last 22,000 years. Through …