Where: Greenland (70.0° N, 52.1° W: paleocoordinates 62.7° N, 22.5° W)
• coordinate based on nearby landmark
• outcrop-level geographic resolution
When: Naujat Member (Atanikerluk Formation), Selandian (61.6 - 59.2 Ma)
• Koch identified the Upper Atanikerdluk A flora and the Upper Atanikerdluk B flora of Heer (1883a, b) in the basal part of the formation (lowermost Naujât Member). A maximum age for the Atanikerluk Formation is obtained from the NP4 – possibly early NP5 marine dinocysts in the underlying Eqalulik Formation (Nøhr-Hansen et al. 2002). Samples from the volcanic Ordlingassoq and Rinks Dal Members give radiometric ages of 60.7–61.1 ± 0.5–1.0 Ma, recalculated from Storey et al. (1998). This indicates an early to mid-Paleocene (possibly Selandian) age for the Atanikerluk Formation.
Environment/lithology: lacustrine; lithified, concretionary, sideritic, black, gray mudstone
•As a result of the opening of the Labrador Sea in Late Mesozoic to Early Cenozoic times, a complex of linked rift basins stretching from the Labrador Sea to northern Baffin Bay developed along West Greenland. Two main episodes of regional rifting and basin development during this time have been documented in the area: an episode of Early Cretaceous rifting, and a Late Cretaceous – Early Paleocene rift episode prior to the start of sea-floor spreading in mid-Paleocene time.
Size class: macrofossils
Preservation: mold/impression
Collected by Steenstrup
• Specimens probably in the Mineralogical Museum, Copenhagen (Steenstrup collection)
Primary reference: O. Heer. 1883. Ueber die fossilen Insekten Grönlands. Flora Fossilis Grönlandica. Die Fossile Flora Grönlands 143-148 [M. Clapham/M. Clapham]more details
Purpose of describing collection: taxonomic analysis
PaleoDB collection 152290: authorized by Matthew Clapham, entered by Matthew Clapham on 16.11.2013
Creative Commons license: CC BY (attribution)
Taxonomic list
Insecta | |
Hydrophilites naujatensis n. sp.
Hydrophilites naujatensis n. sp. Heer 1883 beetle |