Climate Dynamics

, Volume 51, Issue 1–2, pp 667–686 | Cite as

Unraveling the forcings controlling the vegetation and climate of the best orbital analogues for the present interglacial in SW Europe

  • Dulce OliveiraEmail author
  • Stéphanie Desprat
  • Qiuzhen Yin
  • Filipa Naughton
  • Ricardo Trigo
  • Teresa Rodrigues
  • Fátima Abrantes
  • Maria Fernanda Sánchez Goñi


The suitability of MIS 11c and MIS 19c as analogues of our present interglacial and its natural evolution is still debated. Here we examine the regional expression of the Holocene and its orbital analogues over SW Iberia using a model–data comparison approach. Regional tree fraction and climate based on snapshot and transient experiments using the LOVECLIM model are evaluated against the terrestrial–marine profiles from Site U1385 documenting the regional vegetation and climatic changes. The pollen-based reconstructions show a larger forest optimum during the Holocene compared to MIS 11c and MIS 19c, putting into question their analogy in SW Europe. Pollen-based and model results indicate reduced MIS 11c forest cover compared to the Holocene primarily driven by lower winter precipitation, which is critical for Mediterranean forest development. Decreased precipitation was possibly induced by the amplified MIS 11c latitudinal insolation and temperature gradient that shifted the westerlies northwards. In contrast, the reconstructed lower forest optimum at MIS 19c is not reproduced by the simulations probably due to the lack of Eurasian ice sheets and its related feedbacks in the model. Transient experiments with time-varying insolation and CO2 reveal that the SW Iberian forest dynamics over the interglacials are mostly coupled to changes in winter precipitation mainly controlled by precession, CO2 playing a negligible role. Model simulations reproduce the observed persistent vegetation changes at millennial time scales in SW Iberia and the strong forest reductions marking the end of the interglacial “optimum”.


Orbital Holocene analogues Model–data comparison Mediterranean vegetation Marine pollen analysis Insolation CO2 



Financial support was provided by WarmClim, a LEFE-INSU IMAGO project, and the Portuguese Foundation for Science and Technology (FCT) through the project CLIMHOL (PTDC/AAC-CLI/100157/2008), CCMAR (FCT Research Unit—UID/Multi/04326/2013), D. Oliveira’s doctoral grant (SFRH/BD/9079/2012), F. Naughton’s postdoctoral grant (SFRH/BPD/108712/2015) and T. Rodrigues’s postdoctoral grant (SFRH/BPD/108600/2015). Q.Z. Yin is Research Associate of the Belgian National Fund for Scientific Research (FRS-FNRS). This research used samples provided by the Integrated Ocean Drilling Program (IODP), Expedition 339. We would like to thank the scientists and technicians of IODP Expedition 339, the Bremen Core Repository, L. Devaux for technical assistance and V. Hanquiez for drawing Fig. 1. Computational resources have been provided by the supercomputing facilities of the Université catholique de Louvain (CISM/UCL) and the Consortium des Equipements de Calcul Intensif en Fédération Wallonie Bruxelles (CECI) funded by FRS-FNRS. We thank three anonymous reviewers for their constructive and insightful comments.

Supplementary material

382_2017_3948_MOESM1_ESM.png (516 kb)
Fig. S1 Percentage pollen diagram of selected morphotypes and ecological groups from Site U1385 plotted against depth. Ecological groups include Mediterranean forest (MF) which here includes the Mediterranean taxa and all temperate trees and shrub taxa, excluding Pinus, Cedrus and Cupressaceae; Mediterranean taxa: Quercus evergreen-type, Cistus, Olea, Phillyrea and Pistacia; and semi-desert plants: Artemisia, Chenopodiaceae, Ephedra distachya-type and Ephedra fragilis-type. On the right of the diagram are represented the pollen zones and results of the cluster analysis (PNG 515 KB)
382_2017_3948_MOESM2_ESM.docx (13 kb)
Table S1 AMS 14C radiocarbon dates from Site U1385 and calibrated ages (cal yr BP) using the Marine13 calibration curve (Reimer et al. 2013) implemented in CALIB 7.1 (Stuiver and Reimer 1993; (DOCX 12 KB)
382_2017_3948_MOESM3_ESM.docx (14 kb)
Table S2 Description and interpretation of the pollen record from Site U1385 for last 17.5 ka. Pollen zones are designated as following: U1385 (site name)—number of the pollen zone. MF: Mediterranean forest (DOCX 13 KB)
382_2017_3948_MOESM4_ESM.docx (12 kb)
Table S3 Values of Mediterranean forest (MF) and Mediterranean taxa maxima (averaged and absolute) for each interglacial during the interval comprising the major expansion of both ecological groups. For MIS 1 both values from core MD95-2042 and Site U1385 (italic) are given (DOCX 12 KB)


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Copyright information

© Springer-Verlag GmbH Germany 2017

Authors and Affiliations

  • Dulce Oliveira
    • 1
    • 2
    • 3
    • 4
    Email author
  • Stéphanie Desprat
    • 1
    • 2
  • Qiuzhen Yin
    • 5
  • Filipa Naughton
    • 3
    • 4
  • Ricardo Trigo
    • 6
  • Teresa Rodrigues
    • 3
    • 4
  • Fátima Abrantes
    • 3
    • 4
  • Maria Fernanda Sánchez Goñi
    • 1
    • 2
  1. 1.EPHE, PSL Research UniversityPessacFrance
  2. 2.Laboratoire Paléoclimatologie et Paléoenvironnements MarinsUniversity of Bordeaux, EPOC, UMR 5805PessacFrance
  3. 3.Divisão de Geologia e Georecursos MarinhosInstituto Português do Mar e da Atmosfera (IPMA)LisboaPortugal
  4. 4.CCMAR, Centro de Ciências do MarUniversidade do AlgarveFaroPortugal
  5. 5.Georges Lemaître Center for Earth and Climate Research, Earth and Life InstituteUniversité catholique de LouvainLouvain-la-NeuveBelgium
  6. 6.Instituto Dom LuizUniversidade de LisboaLisboaPortugal

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