{
    "o:id": 10342,
    "url": "https://chloe.cnr.it/s/BiDiAr/item/10342",
    "o:resource_template": "Academic Article",
    "o:resource_class": "bibo:AcademicArticle",
    "dcterms:title": [
        "Une reconstitution des climats du dernier cycle climatique à partir des diagrammes polliniques. Comparaison avec les données océaniques et glaciaires"
    ],
    "dcterms:creator": [
        "Bosselin, Bruno"
    ],
    "dcterms:date": [
        "2003"
    ],
    "dcterms:language": [
        "fra"
    ],
    "dcterms:rights": [
        "https://creativecommons.org/licenses/by-nc-nd/4.0/deed.en CC BY-NC-ND 4.0"
    ],
    "dcterms:abstract": [
        "The multivariate treatment of long pollen sequences coming from peat bogs constitutes an easy and effective method of factorial regression for the semi-quantitative reconstruction of the Paleoclimates. The comparison of the results obtained for the upper Pleistocene with the isotopic profiles of sea- and ice-cores, then with the previous methods, confirms a structuralization of the last climatic cycle in four periods: the interglacial Riss/Wurm including the optimum Eemian, the lower pleniglacial, the Wurmian interpleniglacial and the upper pleniglacial, before the Holocene. A numbering system of these oscillations, correlated with the Dansgaard-Oeschger events recognized in the ice-cores of Greenland, is proposed. A final statistical treatment shows a cyclic evolution of the forest vegetation during the Eemian, an evolution which better translates the variations of the Paleoclimates (temperature and humidity) than the arboreal pollen rate (AP)."
    ],
    "dcterms:isPartOf": [
        "https://chloe.cnr.it/s/BiDiAr/item/2002"
    ],
    "bibo:pages": [
        "111–136"
    ],
    "bibo:uri": [
        "http://www.archcalc.cnr.it/journal/id.php?id=356"
    ],
    "bibo:volume": [
        "14"
    ],
    "foaf:homepage": [
        "https://www.zotero.org/groups/5293298/bidiar/items/8HJ3X8KS/item-list"
    ]
},