The medieval climate anomaly and the little Ice Age in coastal Syria inferred from pollen-derived palaeoclimatic patterns
العنوان: | The medieval climate anomaly and the little Ice Age in coastal Syria inferred from pollen-derived palaeoclimatic patterns |
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المؤلفون: | K. Van Lerberghe, E. Van Campo, David Kaniewski, Etienne Paulissen, Harvey Weiss, Ingrid Rossignol, Johan Bakker |
المساهمون: | Laboratoire Ecologie Fonctionnelle et Environnement (ECOLAB), Université Toulouse III - Paul Sabatier (UT3), Université Fédérale Toulouse Midi-Pyrénées-Université Fédérale Toulouse Midi-Pyrénées-Institut Ecologie et Environnement (INEE), Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)-Institut National Polytechnique (Toulouse) (Toulouse INP), Université Fédérale Toulouse Midi-Pyrénées-Observatoire Midi-Pyrénées (OMP), Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Université Fédérale Toulouse Midi-Pyrénées-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Météo France-Centre National d'Études Spatiales [Toulouse] (CNES)-Centre National de la Recherche Scientifique (CNRS)-Institut de Recherche pour le Développement (IRD)-Centre National de la Recherche Scientifique (CNRS) |
المصدر: | Global and Planetary Change Global and Planetary Change, Elsevier, 2011, 78, pp.178-187. ⟨10.1016/j.gloplacha.2011.06.010⟩ |
بيانات النشر: | HAL CCSD, 2011. |
سنة النشر: | 2011 |
مصطلحات موضوعية: | Mediterranean climate, Global and Planetary Change, 010504 meteorology & atmospheric sciences, 15. Life on land, 010502 geochemistry & geophysics, Oceanography, medicine.disease_cause, 01 natural sciences, Proxy (climate), Eastern mediterranean, 13. Climate action, Climatology, Pollen, [SDE]Environmental Sciences, medicine, Famine, Alluvium, Environmental history, Little ice age, Geology, 0105 earth and related environmental sciences |
الوصف: | International audience; The alluvial deposits of a small spring valley near Jableh, in north-western coastal Syria, provides a unique record of environmental history covering the last 1000 years. The pollen-derived climatic proxy inferred from a 315 cm deep core of alluvial deposits suggests that a shift towards wetter climatic conditions occurred from circa (ca.) 1000 to 1250 calibrated (cal) yr AD. This period is situated within the time frame of the Medieval Climate Anomaly. The reconstructed temperature trends show that the warming during this medieval episode was not as high as the modern scores, except for short intervals during the early 12th century AD. The core also recorded a shift towards drier conditions starting during the late 12th century AD, which represents the Eastern Mediterranean expression of the European "Great Famine" climatic event. The main dry and cool interval recorded in coastal Syria occurred from ca. 1520 to 1870 cal yr AD, a time frame encompassing the Little Ice Age. In Mediterranean Syria, the Little Ice Age is not only cooler, but also much drier than the Medieval Climate Anomaly and the present-day climate. Despite a strong human presence in coastal Syria throughout the last millennia, climate rather than anthropogenic activity seems to be the driving force behind the natural vegetation dynamics in this region. |
اللغة: | English |
تدمد: | 0921-8181 |
DOI: | 10.1016/j.gloplacha.2011.06.010⟩ |
URL الوصول: | https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c193b079cb28698d1f8df783fedebf5c https://hal.archives-ouvertes.fr/hal-00959892 |
Rights: | RESTRICTED |
رقم الانضمام: | edsair.doi.dedup.....c193b079cb28698d1f8df783fedebf5c |
قاعدة البيانات: | OpenAIRE |
تدمد: | 09218181 |
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DOI: | 10.1016/j.gloplacha.2011.06.010⟩ |