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Climate of the Past An interactive open-access journal of the European Geosciences Union
https://doi.org/10.5194/cp-2017-104
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 4.0 License.
Research article
24 Aug 2017
Review status
This discussion paper is a preprint. A revision of the manuscript is under review for the journal Climate of the Past (CP).
Holocene aridification trend interrupted by millennial- and centennial-scale climate fluctuations from a new sedimentary record from Padul (Sierra Nevada, southern Iberian Peninsula)
María J. Ramos-Román1, Gonzalo Jiménez-Moreno1, Jon Camuera1, Antonio García-Alix1, R. Scott Anderson2, Francisco J. Jiménez-Espejo3, and José S. Carrión4 1Departamento de Estratigrafía y Paleontología, Universidad de Granada, Spain
2School of Earth Sciences and Environmental Sustainability, Northern Arizona University, USA
3Department of Biogeochemistry, Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Japan
4Departamento de Biología Vegetal, Facultad de Biología, Universidad de Murcia, Murcia, Spain
Abstract. Holocene centennial-scale paleoenvironmental variability has been described in a multiproxy analysis (i.e. lithology, geochemistry, macrofossil and microfossil analyses) of a paleoecological record from the Padul basin in Sierra Nevada, southern Iberian Peninsula. This sequence covers a relevant time interval hitherto unreported in the studies of the Padul sedimentary sequence. The ca. 4700 yr-long record has preserved proxies of climate variability, with vegetation, lake levels and sedimentological change the Holocene in one of the most unique and southernmost peat bogs from Europe. The progressive Middle and Late Holocene trend toward arid conditions identified by numerous authors in the western Mediterranean region, mostly related to a decrease in summer insolation, is also documented in this record, being here also superimposed by centennial-scale variability in humidity. In turn, this record shows centennial-scale climate oscillations in temperature that correlate with well-known climatic events during the Late Holocene in the western Mediterranean region, synchronous with variability in solar and atmospheric dynamics. The multiproxy Padul record first shows a transition from a relatively humid Middle Holocene in the western Mediterranean region to more aridity from ~ 4700 to ~ 2800 cal yr BP. A relatively warm and humid period occurred between ~ 2600 to ~ 1600 cal yr BP, coinciding with persistent negative NAO conditions and the historic Iberian-Roman Humid Period. Enhanced arid conditions, co-occurring with overall positive NAO conditions and increasing solar activity, are observed between ~ 1550 to ~ 450 cal yr BP (~ 400 to ~ 1400 CE) and colder and warmer conditions happened during the Dark Ages and Medieval Climate Anomaly, respectively. Slightly wetter conditions took place during the end of the MCA and the first part of the Little Ice Age, which could be related to a change towards negative NAO conditions and minima in solar activity. Evidences of higher human impact in the Padul peat bog area are observed in the last ~ 1550 cal yr BP. Time series analysis performed from local (Botryococcus and TOC) and regional signals (Mediterranean forest) helped us determining the relationship between southern Iberian climate evolution, atmospheric, oceanic dynamics and solar activity.

Citation: Ramos-Román, M. J., Jiménez-Moreno, G., Camuera, J., García-Alix, A., Anderson, R. S., Jiménez-Espejo, F. J., and Carrión, J. S.: Holocene aridification trend interrupted by millennial- and centennial-scale climate fluctuations from a new sedimentary record from Padul (Sierra Nevada, southern Iberian Peninsula), Clim. Past Discuss., https://doi.org/10.5194/cp-2017-104, in review, 2017.
María J. Ramos-Román et al.
María J. Ramos-Román et al.
María J. Ramos-Román et al.

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Short summary
In this study we carried out a multi-proxy high-resolution analysis on a sediment record from the Padul basin in Sierra Nevada (southern Iberian Peninsula). Padul is a classical and very unique site from the Mediterranean area as it contains a very long and continuos Quaternary sedimentary record. However, the uppermost part of the record was never previously recovered. In this study we focus on the last 4700 cal yr BP of Holocene climate variability and human activity in the Mediterranean area.
In this study we carried out a multi-proxy high-resolution analysis on a sediment record from...
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