Résumés
Abstract
Devonian strata of the present-day Arctic contain abundant and diverse assemblages of terrestrial palynomorphs, particularly from Middle and Upper Devonian sections; few intervals of Lower Devonian and Silurian strata have been palynologically studied, and these demonstrate strong palynofloral similarities across the region. Based on published records, we present a compilation of six last occurrence events (LOs), 44 first occurrence events (FOs) and one acme event that have proven of value in correlation in the present-day Arctic. Although their chronostratigraphic resolution is relatively low, and a scarcity of independent age control hampers precise age assignments, palynology is the only biostratigraphic discipline available for confident chronostratigraphic correlation of most Arctic Devonian strata.
Résumé
Les strates dévoniennes de l’Arctique d’aujourd’hui abritent des assemblages abondants et diversifiés de palynomorphes, terrestres, en particulier des sections du Dévonien moyen et supérieur. Quelques intervalles de strates du Dévonien inférieur et du Silurien ont fait l’objet d’études palynologiques et celles-ci ont révélé des similarités palynoflorales marquées à l’échelle de la région. Nous basant sur des documents publiés, nous présentons une compilation des six dernières occurrences (DO), des 44 premières occurrences (PO) et d’un phénomène d’abondance s’étant avérés utiles pour la corrélation dans l’Arctique d’aujourd’hui. Même si leur résolution chronostratigraphique est relativement faible et que la rareté des contrôles indépendants de la datation gêne l’attribution d’âges précis, la palynologie est la seule discipline biostratigraphique dont nous disposons pour l’établissement d’une corrélation chronostratigraphique sûre de la majorité des strates dévoniennes arctiques.
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