Fur Formation


The Fur Formation is a marine geological formation of Ypresian age which crops out in the Limfjord region of northern Denmark from Silstrup via Mors and Fur to Ertebølle, and can be seen in many cliffs and quarries in the area. The Diatomite Cliffs is on the Danish list of tentative candidates for World Heritage and may become a World Heritage site. Fossils found in the Fur Formation are primarily housed at the Fossil and Mo-clay Museum on Mors Island, the Fur Museum on Fur Island, and the Natural History Museum of Denmark in Copenhagen.

Geology

The Fur Formation is a unit of diatomitic sediment approximately 60 meters thick consisting of diatoms and clay minerals with up to 180 layers of volcanic ash. In Danish literature the formation has informally been referred to as the moler. The diatomite comprises 2/3 opal tests of diatoms and 1/3 clay, interbedded with layers of volcanic ash and a few limestone horizons, and has exceptionally complete fossil preservation.
It is known for its abundant fossil fish, insects, reptiles, birds and plants. The Fur Formation was deposited just above the Palaeocene-Eocene boundary, about 55 million years ago, and its tropical or sub-tropical flora indicate that the climate after the Paleocene-Eocene Thermal Maximum was moderately warm.
Glacial activity has moved and folded all exposed moler in a complicated pattern which permits very precise mapping of glacial movement at the end of the last ice age, and has, due to the ash layers, created an extraordinary pedagogical case for studying tectonics.

Members

The Fur Formation is divided into two members:
The lower Knudeklint Member was named for a location on the island of Fur. The upper Silstrup Member was named for a location in Thy. The stratigraphy exposed at Knudeklint constitutes the unit that containing the Paleocene/Eocene boundary informally named Stolleklint Clay, which grades up into the Fur Formation.

Paleontological significance

Fossils of great diversity and unique preservation Most unusual, if not unique, diversity of life from both ocean and land with extremely good preservation of details rarely seen, therefore very reliable reconstruction of palaeobiology. By far most of the "Danekræ" fossils since 1990 have been found in the Mo-clay area.

Birds

The Fur Formation preserves the earliest diverse Paleogene bird fauna known, with over 30 species, including some near complete, some preserved in 3-D, and some excellent bird-fossils. Most are the earliest known representatives of their orders and all are terrestrial birds.
GenusSpeciesHigher taxonNotesImages
ChascacocoliusC. oscitans?SandcoleidaeOnly known from one wing
EocypselusE. vincentiApodiformesMainly known from the London Clay
Galliformes indet.UnapplicableGalloanseraeKnown from foot imprints distinct from all other Eocene galliforms
LithornisL. vulturinusLithornithidaeFirst complete lithornithid specimen known
MopsittaM. tantaPsittaciformes incertae sedis?Formerly the largest fossil parrot known, however it may actually be synonymous with the ibis Rhynchaeites
MorsoravisM. sedilisMorsoravidaeFormerly classed as a charadriiform before being reclassified as a basal member of Psittacopasseres
Halcyornithidae indet.UnapplicableEufalconimorphaeOnly known from one humerus
PellornisP. mikkelseniMesselornithidaeLimb specialisation indicates it was likely cursorial, redescribed from several complete skeletons which support it being a crown-gruiform
ScandiavisS. mikkelseniCharadriiformes?Likely a basal member due to features of the postcrania
SeptencoraciasS. morsensisCoraciiformesOne of the earliest rollers, preserved with fish in its stomach
SeptentrogonS. madseniTrogonidaeEarliest trogon known

Reptiles

Several fossil sea turtles are known from the Fur Formation. In one of them, a large leatherback turtle remains of soft tissue and skin pigmentation have been recovered A number of well-preserved turtle specimens have been recovered from the formation, two of which have been recognized to be a completely new species of the genus Tasbacka.
Sea snakes are also known from the formation.
Large teleostean fauna, oceanic, possibly including earliest truly deepwater fish, a 'whale-fish'; earliest members of many living families and Tertiary diversity preserved as complete skeletons; some rare and sensational large and complete specimens.
The following taxa are known:
GenusSpeciesLocationMemberNotesImages
?Analectis?A. sp.FurA turkmenid lampriform.
?Antigonia?A. sp.FurA boarfish.
ArchaeozeusA. skamolensisFurAn archaeozeid zeiform.
?Arius?A. sp.FurA sea catfish.
Atheriniformes indet.FurAn atheriniform.
Aulostomoidea indet.FurAn aulostomoid.
BrychaetoidesB. greenwoodiFurA bonytongue.
cf. BrychaetusB. sp.Stolle KlintA bonytongue.
ButyrumichthysB. henriciiFurA medusafish.
Euzaphlegidae indet.FurA euzaphlegid.
ExelliaE. sp.FurAn exelliid percomorph.
FurichthysF. fieldsoeiFurA bonytongue.
HeterosteoglossumH. foreyiFur, Stolle KlintA bonytongue.
HolosteusH. sp.FurA barracudina.
Megalopidae indet.FurA tarpon.
MeneM. sp.FurA moonfish.
MoclaybalistesM. danekrusFurA moclaybalistid tetraodontiform.
Muraenidae indet.FurA moray eel.
Osteoglossiformes indet.FurA small-sized osteoglossiform.
PalaeocentrotusP. boeggildiFurA palaeocentrotid lampriform.
Palaeorhynchidae indet.FurA billfish.
?Percopsiformes indet.FurA potential percopsiform.
PolyspinatusP. fluereFurA beardfish.
ProtozeusP. kuehneiFurA protozeid zeiform.
RhamphosusR. sp.FurA syngnathiform.
RhinocephalusR. sp.FurA hake.
?Rondeletia?R. sp.FurA whalefish, possibly a redmouth whalefish.
?Salmonidae indet.FurA potential salmonid.
?Sardinella?S. sp.FurA clupeid.
?Scorpaeniformes indet.FurA potential scorpaeniform.
SurlykusS. longigracilisFurAn argentiniform, the most common fish in the Mo-Clay.
?Vomeropsis?V. sp.FurA carangid.
XosteoglossidX. rebeccaeStolle KlintA bonytongue.

Insects

Huge fauna from land, over 200 species, many are oldest of their families; many with colour spots and eye lenses, some extraordinary preservation with stridulation apparatus in grasshoppers, and apparently migratory moth mass mortality.
GenusSpeciesHigher taxonNotesImages
ApachyusA. madseniApachyidaeFirst fossil apachyid
CephalallusC. vitaliiSpondylidinaeFirst longhorn beetle from the formation
CryptocheilusC. lelejiPepsiniEarliest pompillid wasp known
DanoberothaD. verkleijorumBerothidaeFirst berothid from the formation
DanochrysaD. madseniChrysopidae
DanolestesD. moelleriLestoideaA member of Lestoidea of uncertain affinities.
DanomantispaD. frandseniMantispidaeIntermediate between Drepanicinae and Mantispinae
EodysagrionE. mikkelseniDysagrionidae Member of its own subfamily, Eodysagrioninae
EosassulaE. szwedoiNogodinidaeOne of the few nogodinid fossils
FuragrionF. jutlandicusZygopteraBears all wing venation characters of cephalozygopterans, but has a head similar to zygopterans
FurochrysaF. alisaeChrysopidaeDistinguished by a long crossvein
MesypochrysaM. nielseniChrysopidaeLatest record of the Mesozoic genus Mesypochrysa-
PachycondylaP. rebekkaePonerinaeOne of the earliest fossil ants in an extant genus at the time of description
PalaeopsychopsP. quadratusPolystoechotidaeBears stripes along its crossveins
ParabaissaeshnaP. ejerslevenseAeshnidaeResembles the Mesozoic Baissaeshna
PseudotettigoniaP. amoenaTettigoniidaePreserves a complete stridulatory organ, with the structure of the organ suggesting that it was able to hear low ultrasound
PrimorilestesP. madseniDysagrionidae
ProtheristriaP. roldaeMantispidaeIn the same subfamily as the other mantisfly known from the formation, but otherwise unrelated
RhantusR. villumiDytiscidaeOldest species in the genus
StephenbrooksiaS. multifurcataChrysopidaeBears unusual hind wing venation
StolleagrionS. foghnielseniCephalozygoptera First odonate known from the early Ypresian
TriachrysaT. rustiChrysopidaeHas three series of crossveins in its wings, alongside several unrelated genera