A preliminary report on coprolites from the Late Triassic part of the Kap Stewart Formation, Jameson Land, East Greenland

Research output: Contribution to journalJournal articleResearchpeer-review

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A preliminary report on coprolites from the Late Triassic part of the Kap Stewart Formation, Jameson Land, East Greenland. / Milàn, Jesper; Clemmensen, Lars B; Adolphsen, Jan Schulz; Estrup, Eliza Jarl; Frobøse, Nicolai; Klein, Nicole; Mateus, Octavio; Wings, Oliver.

In: New Mexico Museum of Natural History and Science. Bulletin, Vol. 57, 2012, p. 203-205.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Milàn, J, Clemmensen, LB, Adolphsen, JS, Estrup, EJ, Frobøse, N, Klein, N, Mateus, O & Wings, O 2012, 'A preliminary report on coprolites from the Late Triassic part of the Kap Stewart Formation, Jameson Land, East Greenland', New Mexico Museum of Natural History and Science. Bulletin, vol. 57, pp. 203-205.

APA

Milàn, J., Clemmensen, L. B., Adolphsen, J. S., Estrup, E. J., Frobøse, N., Klein, N., Mateus, O., & Wings, O. (2012). A preliminary report on coprolites from the Late Triassic part of the Kap Stewart Formation, Jameson Land, East Greenland. New Mexico Museum of Natural History and Science. Bulletin, 57, 203-205.

Vancouver

Milàn J, Clemmensen LB, Adolphsen JS, Estrup EJ, Frobøse N, Klein N et al. A preliminary report on coprolites from the Late Triassic part of the Kap Stewart Formation, Jameson Land, East Greenland. New Mexico Museum of Natural History and Science. Bulletin. 2012;57:203-205.

Author

Milàn, Jesper ; Clemmensen, Lars B ; Adolphsen, Jan Schulz ; Estrup, Eliza Jarl ; Frobøse, Nicolai ; Klein, Nicole ; Mateus, Octavio ; Wings, Oliver. / A preliminary report on coprolites from the Late Triassic part of the Kap Stewart Formation, Jameson Land, East Greenland. In: New Mexico Museum of Natural History and Science. Bulletin. 2012 ; Vol. 57. pp. 203-205.

Bibtex

@article{a7ab241398824a6581132d886f175d94,
title = "A preliminary report on coprolites from the Late Triassic part of the Kap Stewart Formation, Jameson Land, East Greenland",
abstract = "The basal part of the Triassic-Jurassic (Rhaetian-Sinemurian) Kap Stewart Formation, exposed at Jameson Land, East Greenland, yields an extensive coprolite collection from black, parallel-laminated mudstone (“paper shale”), representing an open lacustrine system. Preliminary investigations show three different types ofcoprolites: elongated cylindrical masses, composed of irregularly wrapped layers; elongated cylindrical masses with constriction marks; and spirally-coiled specimens.",
author = "Jesper Mil{\`a}n and Clemmensen, {Lars B} and Adolphsen, {Jan Schulz} and Estrup, {Eliza Jarl} and Nicolai Frob{\o}se and Nicole Klein and Octavio Mateus and Oliver Wings",
year = "2012",
language = "English",
volume = "57",
pages = "203--205",
journal = "New Mexico Museum of Natural History and Science. Bulletin",
issn = "1524-4156",

}

RIS

TY - JOUR

T1 - A preliminary report on coprolites from the Late Triassic part of the Kap Stewart Formation, Jameson Land, East Greenland

AU - Milàn, Jesper

AU - Clemmensen, Lars B

AU - Adolphsen, Jan Schulz

AU - Estrup, Eliza Jarl

AU - Frobøse, Nicolai

AU - Klein, Nicole

AU - Mateus, Octavio

AU - Wings, Oliver

PY - 2012

Y1 - 2012

N2 - The basal part of the Triassic-Jurassic (Rhaetian-Sinemurian) Kap Stewart Formation, exposed at Jameson Land, East Greenland, yields an extensive coprolite collection from black, parallel-laminated mudstone (“paper shale”), representing an open lacustrine system. Preliminary investigations show three different types ofcoprolites: elongated cylindrical masses, composed of irregularly wrapped layers; elongated cylindrical masses with constriction marks; and spirally-coiled specimens.

AB - The basal part of the Triassic-Jurassic (Rhaetian-Sinemurian) Kap Stewart Formation, exposed at Jameson Land, East Greenland, yields an extensive coprolite collection from black, parallel-laminated mudstone (“paper shale”), representing an open lacustrine system. Preliminary investigations show three different types ofcoprolites: elongated cylindrical masses, composed of irregularly wrapped layers; elongated cylindrical masses with constriction marks; and spirally-coiled specimens.

M3 - Journal article

VL - 57

SP - 203

EP - 205

JO - New Mexico Museum of Natural History and Science. Bulletin

JF - New Mexico Museum of Natural History and Science. Bulletin

SN - 1524-4156

ER -

ID: 44163409