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Maastricht - Valkenburg

FormationMaastricht
MemberValkenburg
Age:70.6 - 66.0 Ma
Late/Upper Cretaceous
IntervalLate Maastrichtian
Lithologychalk, lime mudstone, grainstone
Number of Collections6
Number of Occurrences13

Recorded Sample Locations

LocationRegionStratigraphic Name
Ankerpoort-Marnebel quarry Bassenge, Liège, Wallonia, BelgiumMaastricht - Valkenburg
Valkenburg ChalkValkenburg aan de Geul, Limburg, NetherlandsMaastricht - Valkenburg
Blankenberg QuarryLimburg, NetherlandsMaastricht - Valkenburg
EchinodermsBassenge, Liège, Wallonia, BelgiumMaastricht - Valkenburg
ENCILimburg, NetherlandsMaastricht - Valkenburg

Associated Units

Stratigraphic NameAgeLithologyOccurrence Records
Gulpen - Lanaye70.6 - 66.0 Ma
Late/Upper Cretaceous
wackestone, "limestone", grainstone, chert82
Maastricht - Emael70.6 - 66.0 Ma
Late/Upper Cretaceous
packstone, chalk, "limestone"76
Maastricht - Gronsveld70.6 - 66.0 Ma
Late/Upper Cretaceous
chalk2
Maastricht - Gronsveld, Schiepersberg70.6 - 66.0 Ma
Late/Upper Cretaceous
packstone8
Maastricht - Meerssen66.0 - 61.6 Ma
Paleocene
grainstone, packstone, "limestone", chalk271
Maastricht - Nekum70.6 - 66.0 Ma
Late/Upper Cretaceous
packstone, grainstone, chalk, lime mudstone, "limestone", chert113
Maastricht - Valkenburg, Gronsveld72.1 - 66.0 Ma
Late/Upper Cretaceous
packstone45

Recorded Fossils

Accepted NameHierarchyAge
Thalassotaenia debeyi
species
7Thalassotaenia : Thalassotaenia debeyi70.6 - 66 Ma
Late/Upper Cretaceous
Veenia sp.
genus
6Animalia : Arthropoda : Ostracoda : Podocopida : Trachyleberididae : Veenia70.6 - 66 Ma
Late/Upper Cretaceous
Eolacazella sp.
genus
6Animalia : Brachiopoda : Rhynchonellata : Thecideida : Thecideidae : Eolacazella70.6 - 66 Ma
Late/Upper Cretaceous
Ornithurae
subclass
3.3Animalia : Chordata : Aves : Ornithurae70.6 - 66 Ma
Late/Upper Cretaceous
Maastrichtidelphys meurismeti
species
7Animalia : Chordata : Mammalia : Didelphimorphia : Peradectidae : Maastrichtidelphys : Maastrichtidelphys meurismeti70.6 - 66 Ma
Late/Upper Cretaceous
Hadrosauridae
family
5Animalia : Chordata : Reptilia : Dinosauria : Hadrosauridae70.6 - 66 Ma
Late/Upper Cretaceous
Baculites sp.
genus
6Animalia : Mollusca : Cephalopoda : Ammonoidea : Baculitidae : Baculites70.6 - 66 Ma
Late/Upper Cretaceous
Baculites anceps
species
7Animalia : Mollusca : Cephalopoda : Ammonoidea : Baculitidae : Baculites : Baculites anceps70.6 - 66 Ma
Late/Upper Cretaceous
Belemnella sp.
genus
6Animalia : Mollusca : Cephalopoda : Belemnitida : Belemnella70.6 - 66 Ma
Late/Upper Cretaceous

References

Kennedy W. J. (1986) The ammonite fauna of the type Maastrichtian with a revision of Ammonites colligatus Binkhorst, 1861, Bull. Inst. r. Sci. nat. Belg.: Science de la Terre 56, 151-267
Kennedy W. J. (1986) The Campanian-Maastrichtian ammonite sequence in the environs of Maastricht (Limburg, the Netherlands), Limburg and Liége provinces (Belgium), Newsletters in Stratigraphy 16 3, 149-168
Jagt J. W. M., Dortangs R. W., et al (1998) Dinosaur remains in the type Maastrichtian: an update, In J. W. M. Jagt, P. H. Lambers, E. W. A. Mulder & A. Schulp (eds), Third European Workshop on Vertebrate Palaeontology, Maastricht, Netherlands. Natuurhistorisch Museum Maastricht
Dyke G. J., Dortangs R. W., et al (2002) Europe's last Mesozoic bird, Naturwissenschaften 89, 408-411
Leloux J. (2002) Type specimens of Maastrichtian fossils in the National Museum of Natural History, Leiden
Martin J. E., Case J. A., et al (2005) A new European marsupial indicates a Late Cretaceous high-latitude transatlantic dispersal route, Journal of Mammalian Evolution 12 3/4, 495-511
van der Ham R. W. J., van Konijnenburg-van Cittert J. H. A., et al (2007) Seagrass foliage from the Maastrichtian type area (Maastrichtian, Danian, NE Belgium, SE Netherlands), Review of Palaeobotany and Palynology 144 3-4, 301-321
Data courtesy of: PBDB: The Paleobiology Database, Creative Commons CC-BY licenced. , GBIF: the Global Biodiversity Information Facility, various licences, iDigBio, various licences, and EOL: The Encyclopedia of Life (Open Data Public Domain). Because fossils are made of minerals too!
 
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