This article reviews key data and debates focused on relative sea-level changes since the
Last Interglacial (approximately the last 132,000 years) in the Mediterranean Basin, and …

The dust cycle is an integral part of the Earth system. Each year, an estimated 2000 Mt dust
is emitted into the atmosphere, 75% of which is deposited to the land and 25% to the ocean …

Dust storms, produced by the removal of surface materials from the world's drylands, are a
vital component of the environment. This is because of their role in biogeochemical cycling …

Dust storms have a number of impacts upon the environment including radiative forcing, and
biogeochemical cycling. They transport material over many thousands of kilometres. They …

Selected multi-proxy and accurately dated marine and terrestrial records covering the past
2000 years in the Iberian Peninsula (IP) facilitated a comprehensive regional paleoclimate …

High-resolution pollen analysis of Alborán Sea core MD95-2043 provides a 48-ka
continuous vegetation record that can be directly correlated with sea surface and deep …

Marine sediments record paleoenvironmental changes over time through variations in major
and trace element concentrations. The main objective of this paper is to review such …

One of the outstanding problems of palaeoclimate reconstruction from physico-chemical
properties of terrigenous deep-sea sediments stems from the fact that most basin fills are …

Population models seeking climate as a triggering factor for the extinction of Neandertals
and the colonisation of Europe by Anatomically Modern Humans are contradictory due to …

Palynological, sedimentological and stable isotopic analyses of carbonates and organic
matter performed on the El Portalet sequence (1802 m asl, 42° 48′ 00ʺN, 0° 23′ 52ʺW) …