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A snapshot into the terrestrial ecosystem of an exceptionally well-preserved dinosaur (Hadrosauridae) from the Upper Cretaceous of North Dakota, USA

Vajda, Vivi LU ; Lyson, Tylor ; Bercovici, Antoine LU ; Doman, Jessamy and Pearson, Dean (2013) In Cretaceous Research 46. p.114-122
Abstract
A palynological investigation of sedimentary rocks enclosing an exceptionally well-preserved fossil

dinosaur (Hadrosauridae) discovered in the upper part of the Hell Creek Formation in south western

North Dakota was conducted in order to document the immediate paleoenvironment of this dinosaur.

The specimen, an Edmontosaurus annectens is remarkable in having exceptional three-dimensional

preservation of soft tissue around the skeleton, indicating rapid burial. A well-preserved palynological

assemblage dominated by fern and bryophyte spores, with lesser gymnosperm and angiosperm pollen

was recovered. Sparse fresh-water algae and marine dinoflagellate cysts were also recorded. The... (More)
A palynological investigation of sedimentary rocks enclosing an exceptionally well-preserved fossil

dinosaur (Hadrosauridae) discovered in the upper part of the Hell Creek Formation in south western

North Dakota was conducted in order to document the immediate paleoenvironment of this dinosaur.

The specimen, an Edmontosaurus annectens is remarkable in having exceptional three-dimensional

preservation of soft tissue around the skeleton, indicating rapid burial. A well-preserved palynological

assemblage dominated by fern and bryophyte spores, with lesser gymnosperm and angiosperm pollen

was recovered. Sparse fresh-water algae and marine dinoflagellate cysts were also recorded. The palynofacies

is dominated by wood fragments, including charcoal, with little amorphous organic matter. The

presence of some typical pollen taxa of the Wodehouseia spinata Assemblage Zone including Striatellipollis

striatellus, Tricolpites microreticulatus, Leptopecopites pocockii as well as a diverse suite of Aquilapollenites,is fully consistent with a Late Cretaceous (late Maastrichtian) age. The palynoflora indicates a local vegetation composed of a canopy of conifers dominated by Pinaceae and a minor sub-canopy of Taxodium and cycads, as well as an understory of hydrophilous ferns, mosses and herbaceous angiosperms,indicative of a warm and humid climate e an environment where this specific hadrosaur roamed over 66 million years ago. (Less)
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author
; ; ; and
organization
publishing date
type
Contribution to journal
publication status
published
subject
keywords
Hell Creek, Maastrichtian, paleoclimate, palynology, Hadrosaur, dinosaur, swamp
in
Cretaceous Research
volume
46
pages
114 - 122
publisher
Elsevier
external identifiers
  • wos:000329553900011
  • scopus:84886775423
ISSN
0195-6671
DOI
10.1016/j.cretres.2013.08.010
language
English
LU publication?
yes
id
31c8da75-21e3-4e37-8c73-08b6a4193217 (old id 4281165)
date added to LUP
2016-04-01 14:22:01
date last changed
2022-01-28 00:13:13
@article{31c8da75-21e3-4e37-8c73-08b6a4193217,
  abstract     = {{A palynological investigation of sedimentary rocks enclosing an exceptionally well-preserved fossil<br/><br>
dinosaur (Hadrosauridae) discovered in the upper part of the Hell Creek Formation in south western<br/><br>
North Dakota was conducted in order to document the immediate paleoenvironment of this dinosaur.<br/><br>
The specimen, an Edmontosaurus annectens is remarkable in having exceptional three-dimensional<br/><br>
preservation of soft tissue around the skeleton, indicating rapid burial. A well-preserved palynological<br/><br>
assemblage dominated by fern and bryophyte spores, with lesser gymnosperm and angiosperm pollen<br/><br>
was recovered. Sparse fresh-water algae and marine dinoflagellate cysts were also recorded. The palynofacies<br/><br>
is dominated by wood fragments, including charcoal, with little amorphous organic matter. The<br/><br>
presence of some typical pollen taxa of the Wodehouseia spinata Assemblage Zone including Striatellipollis<br/><br>
striatellus, Tricolpites microreticulatus, Leptopecopites pocockii as well as a diverse suite of Aquilapollenites,is fully consistent with a Late Cretaceous (late Maastrichtian) age. The palynoflora indicates a local vegetation composed of a canopy of conifers dominated by Pinaceae and a minor sub-canopy of Taxodium and cycads, as well as an understory of hydrophilous ferns, mosses and herbaceous angiosperms,indicative of a warm and humid climate e an environment where this specific hadrosaur roamed over 66 million years ago.}},
  author       = {{Vajda, Vivi and Lyson, Tylor and Bercovici, Antoine and Doman, Jessamy and Pearson, Dean}},
  issn         = {{0195-6671}},
  keywords     = {{Hell Creek; Maastrichtian; paleoclimate; palynology; Hadrosaur; dinosaur; swamp}},
  language     = {{eng}},
  pages        = {{114--122}},
  publisher    = {{Elsevier}},
  series       = {{Cretaceous Research}},
  title        = {{A snapshot into the terrestrial ecosystem of an exceptionally well-preserved dinosaur (Hadrosauridae) from the Upper Cretaceous of North Dakota, USA}},
  url          = {{http://dx.doi.org/10.1016/j.cretres.2013.08.010}},
  doi          = {{10.1016/j.cretres.2013.08.010}},
  volume       = {{46}},
  year         = {{2013}},
}