Mario Morellón

TL;DR: In this article, the authors presented a comprehensive regional paleoclimate reconstruction for the Medieval Climate Anomaly (MCA: 900-1300 AD) in the Mediterranean IP using multi-proxy and accurately dated marine and terrestrial records covering the past 2000 years.

TL;DR: In this paper, the authors explored how the North Atlantic Oscillation and other atmospheric circulation modes operated over the longer timescales of the Medieval Climate Anomaly (MCA) and Little Ice Age (LIA) and used high-resolution palaeolimnological evidence from opposite ends of the Mediterranean basin, supplemented by other palaeoclimate data, to track shifts in regional hydro-climatic conditions.

TL;DR: In this article, a multiresolution analysis of sediment cores recovered in karstic Lake Estanya (42°02′ N, 0°32′ E; 670 m a. s. l., NE Spain), located in the transitional area between the humid Pyrenees and the semi-arid Central Ebro Basin, provides the first high-resolution, continuous sedimentary record in the region, extending back the last 21,000 years.

TL;DR: A multi-proxy study of short sediment cores recovered in small, karstic Lake Estanya (42°02′N, 0°32′E, 670 m.a.s.l.) in the Pre-Pyrenean Ranges (NE Spain) provides a detailed record of the complex environmental, hydrological and anthropogenic interactions occurring in the area since medieval times as discussed by the authors.

TL;DR: This article presented a palaeoclimatic reconstruction of the last glacial cycle in Iberia (ca 120,000 to 11,600 cal yrs BP) based on multi-proxy reconstructions from lake sediments with robust chronologies, with a particular focus on abrupt climate changes.