Knude Klint (Knuden), Fur (Eocene of Denmark)

Where: Denmark (56.8° N, 9.0° E: paleocoordinates 52.4° N, 5.6° E)

• coordinate estimated from map

• small collection-level geographic resolution

When: Fur Formation, Ypresian (56.0 - 47.8 Ma)

• Specimens are from between ash layers +28 & +24

•Earliest Early Eocene "An Early Eocene age of 54.04 ± 0.14 Ma has been determined for layer +19 and 54.52 ± 0.05 Ma for layer −17 by the Ar40–Ar39 method (Chambers et al. 2003).

Environment/lithology: offshore ramp; lithified diatomite and carbonate

• The depositional environment was in the Palaeocene–Eocene precursor of the North Sea, which was an almost or entirely enclosed inland body, open to the Atlantic at least at times (Bonde 1997).
• striated cement stone

•"The Danish insects discussed here are from the marine Fur Formation, about 50-60 m of diatomite and tephra layers, which, with the Ølst Formation, constitute the Mo-clay in the northern Jutland region" Archibald & Makarkin, 2006

Size classes: macrofossils, mesofossils

Preservation: adpression

Collection methods: Repository: Geological (Mineralogical) Museum, University of Copenhagen

Primary reference: O. E. Heie. 1967. Studies on fossil aphids (Homoptera: Aphidoidea), especially in the Copenhagen collection of fossils in Baltic amber. Spolia Zoologica Musei Hauniensis 26:1-274 [M. Clapham/A. Noshirvan/M. Clapham]more details

Purpose of describing collection: taxonomic analysis

PaleoDB collection 120020: authorized by Matthew Clapham, entered by Jered Karr on 06.11.2011, edited by Matthew Clapham

Creative Commons license: CC BY (attribution)

Taxonomic list

Insecta
 Diptera - Tipulidae
Tipula limfjordensis1 Freiwald 1990 crane fly
KM 86A, 793 (horizon E)
 Hemiptera - Aphididae
Diatomyzus eocaenicus n. gen. n. sp.2 Heie 1970 aphid
M4 is holotype M5-M6 are tentatively referred
Siphonophoroides magnalata n. sp. Heie 1967 aphid
M-3