Strong continentality and effective moisture drove unforeseen vegetation dynamics since the last interglacial at inland Mediterranean areas: The Villarquemado sequence in NE Iberia

P. González-Sampériz, G. Gil-Romera, E. García-Prieto, J. Aranbarri, A. Moreno, M. Morellón, M. Sevilla-Callejo, M. Leunda, L. Santos, F. Franco-Múgica, A. Andrade, J. S. Carrión, B. L. Valero-Garcés

Research output: Contribution to journalArticlepeer-review

Abstract

Few continental palaeoenvironmental sedimentary sequences from Southern Europe are long enough to span the last interglacial period (Marine Isotopic Stage-MIS 5), the last glacial cycle (MIS 4 to 2) and the Holocene. El Cañizar de Villarquemado (North-Eastern Iberian Peninsula) is an exceptional sedimentary lacustrine sequence spanning the last ca. 135,000 years of environmental change in an area of inland Iberia characterized by Mediterranean climate with strong continentality. We present a multiproxy study which combines palynological, sedimentological and geochemical analyses framed by an independent, robust chronology. Hydrological and climate evolutions were reconstructed by sedimentological and geochemical proxies. Development of wetlands and shallow carbonate lakes support relatively humid conditions during MIS 6, till the onset of MIS 4, and during the Holocene. Palaeohydrological conditions were drier during MIS 5 (dominance of peat environments) than during the Holocene (more frequent carbonate-producing lakes). Sedimentological evidence indicates extremely arid conditions during MIS 3 with greater activity of alluvial fans prograding into the basin. Sedimentary facies variability highlights a large environmental and hydrological variability during MIS 2 and a rapid humidity response to the onset of the Holocene. Compared to classic Mediterranean sites, we found novel pollen assemblages for the end of MIS 6 and MIS 5 indicating that the vegetation cover was essentially represented by sustained high proportions of continentality-adapted taxa dominated by Juniperus during the relatively humid conditions since MIS 6 till the onset of MIS 4. Higher evapotranspiration in inland Iberia would have increased during periods of higher seasonal insolation maxima, impeding soil development and the usual mesophyte expansion during interglacials observed in other Mediterranean areas. Four main periods of forest development occurred in Villarquemado during MIS 5e, MIS 5c, MIS 5a and the Holocene; secondary peaks occurred also during MIS 3. During colder but still relatively humid MIS 4, junipers and Mediterranean taxa disappear but some mesophytes and cold-tolerant species persisted and Pinus became the dominant tree up to modern times. Pollen assemblages and geochemical data variability suggest a dominant control of seasonality and the impact of North Atlantic dynamics both during MIS 5 (cold events C18-C24) and full glacial conditions (HE and D-O interstadials). At millennial scales, steppe herbaceous assemblages dominated during the extremely arid conditions of MIS 3 and pines and steppe taxa during glacial period MIS 2. Villarquemado sequence demonstrates that the resilient behaviour of conifers in continental areas of inland Southern European regions is key to understand the glacial–interglacial vegetation evolution and to evaluate scenarios for potential impacts of global change.

Original languageEnglish (US)
Article number106425
JournalQuaternary Science Reviews
Volume242
DOIs
StatePublished - Aug 15 2020

Bibliographical note

Funding Information:
Funding for this research was provided by the Spanish Inter-Ministry Commission of Science and Technology (CICYT) through the projects DINAMO3 ( CGL2015-69160-R ), DINAMO2 ( CGL2012-33063 ) and DINAMO ( CGL2009-07992 ), as well as the Aragón Regional Government support with project DGA P196/2005 and E02_17R “Geo-environmental Processes and Global Change Group”. Eduardo García-Prieto and Maria Leunda were supported by two PhD fellowship provided by the Spanish Ministry (FPI ref.: BES-2010-038593 and BES-2013-063753 , respectively). Graciela Gil-Romera is funded by the DFG Research Unit FOR2358 “Mountain Exite Hypothesis”. We thank Noemí Fuentes, Beatriz Bueno, Aída Adsuar, Elena Royo and Raquel López Cantero for the help provided during sediment sampling and laboratory procedures. We thank Judy Allen and Jon Camuera, as well as the Neotoma database for provide palynological data for comparison. This work would not have been possible without the help of the “Laguna del Cañizar Foundation” directed by José Carlos Rubio.

Publisher Copyright:
© 2020 Elsevier Ltd

Copyright:
Copyright 2020 Elsevier B.V., All rights reserved.

Keywords

  • Continentality
  • Glacial cycle
  • Iberian Peninsula
  • Interglacial
  • Juniperus
  • Palaeoecology
  • Palynology
  • Pleistocene

Continental Scientific Drilling Facility tags

  • TERUEL

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