Diverse tetrapod trackways in the Lower Pennsylvanian Tynemouth Creek Formation, near St. Martins, southern New Brunswick, Canada

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Diverse tetrapod trackways in the Lower Pennsylvanian Tynemouth Creek Formation, near St. Martins, southern New Brunswick, Canada. / Falcon-Lang, Howard J.; Gibling, Martin R.; Benton, Michael J.; Miller, Randall F.; Bashforth, Arden Roy.

In: Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences, Vol. 296, No. 1-2, 2010, p. 1-13.

Research output: Contribution to journalJournal articleResearchpeer-review

Harvard

Falcon-Lang, HJ, Gibling, MR, Benton, MJ, Miller, RF & Bashforth, AR 2010, 'Diverse tetrapod trackways in the Lower Pennsylvanian Tynemouth Creek Formation, near St. Martins, southern New Brunswick, Canada', Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences, vol. 296, no. 1-2, pp. 1-13. https://doi.org/10.1016/j.palaeo.2010.06.020

APA

Falcon-Lang, H. J., Gibling, M. R., Benton, M. J., Miller, R. F., & Bashforth, A. R. (2010). Diverse tetrapod trackways in the Lower Pennsylvanian Tynemouth Creek Formation, near St. Martins, southern New Brunswick, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences, 296(1-2), 1-13. https://doi.org/10.1016/j.palaeo.2010.06.020

Vancouver

Falcon-Lang HJ, Gibling MR, Benton MJ, Miller RF, Bashforth AR. Diverse tetrapod trackways in the Lower Pennsylvanian Tynemouth Creek Formation, near St. Martins, southern New Brunswick, Canada. Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences. 2010;296(1-2):1-13. https://doi.org/10.1016/j.palaeo.2010.06.020

Author

Falcon-Lang, Howard J. ; Gibling, Martin R. ; Benton, Michael J. ; Miller, Randall F. ; Bashforth, Arden Roy. / Diverse tetrapod trackways in the Lower Pennsylvanian Tynemouth Creek Formation, near St. Martins, southern New Brunswick, Canada. In: Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences. 2010 ; Vol. 296, No. 1-2. pp. 1-13.

Bibtex

@article{2c0b5a30cfa111df825b000ea68e967b,
title = "Diverse tetrapod trackways in the Lower Pennsylvanian Tynemouth Creek Formation, near St. Martins, southern New Brunswick, Canada",
abstract = "Newly discovered tetrapod trackways are reported from eight sites in the Lower Pennsylvanian Tynemouth Creek Formation of southern New Brunswick, Canada. By far the most abundant and well-preserved tracks comprise pentadactyl footprints of medium size (32–53 mm long) with slender digits and a narrow splay (mostly b55°). Digit lengths typically approximate a phalangeal formula of 23453 (manus) and 23454 (pes), but this may vary due to extramorphology. These tracks are referred to Pseudobradypus and they are attributed to early amniotes. A second type of track (rare) comprises very small (5–8 mm long) tetradactyl manus, and incompletely preserved pedes. Referred to Batrachichnus, these are attributed to temnospondyl amphibians. A third type (also rare) comprises small pentadactyl pedes (20–25 mm long) showing stubby, widely splayed (152°) digits with a terminal bulge. Manus are probably pentadactyl (preservation incomplete) with a narrower digit splay. These footprints, classified as Baropezia, are attributed to anthracosaurs. Facies analysis at the mostprolific site (179 footprints documented) suggests that the tetrapods lived amongst small alethopterid trees colonizing the abandoned floor of a seasonally active fixed-channel river and a similar dryland context is probable for the seven other sites. The dominance of amniotes in these dryland alluvial facies contrastsmarkedly with coeval wetland facies in the nearby Joggins Formation, where skeletal and trackway assemblages are amphibian-dominated. This may imply that amniotes were better adapted to seasonally dry settings and sheds new light on the community ecology of tetrapods during a key evolutionary phase.",
author = "Falcon-Lang, {Howard J.} and Gibling, {Martin R.} and Benton, {Michael J.} and Miller, {Randall F.} and Bashforth, {Arden Roy}",
year = "2010",
doi = "10.1016/j.palaeo.2010.06.020",
language = "English",
volume = "296",
pages = "1--13",
journal = "Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences",
issn = "0031-0182",
publisher = "Elsevier",
number = "1-2",

}

RIS

TY - JOUR

T1 - Diverse tetrapod trackways in the Lower Pennsylvanian Tynemouth Creek Formation, near St. Martins, southern New Brunswick, Canada

AU - Falcon-Lang, Howard J.

AU - Gibling, Martin R.

AU - Benton, Michael J.

AU - Miller, Randall F.

AU - Bashforth, Arden Roy

PY - 2010

Y1 - 2010

N2 - Newly discovered tetrapod trackways are reported from eight sites in the Lower Pennsylvanian Tynemouth Creek Formation of southern New Brunswick, Canada. By far the most abundant and well-preserved tracks comprise pentadactyl footprints of medium size (32–53 mm long) with slender digits and a narrow splay (mostly b55°). Digit lengths typically approximate a phalangeal formula of 23453 (manus) and 23454 (pes), but this may vary due to extramorphology. These tracks are referred to Pseudobradypus and they are attributed to early amniotes. A second type of track (rare) comprises very small (5–8 mm long) tetradactyl manus, and incompletely preserved pedes. Referred to Batrachichnus, these are attributed to temnospondyl amphibians. A third type (also rare) comprises small pentadactyl pedes (20–25 mm long) showing stubby, widely splayed (152°) digits with a terminal bulge. Manus are probably pentadactyl (preservation incomplete) with a narrower digit splay. These footprints, classified as Baropezia, are attributed to anthracosaurs. Facies analysis at the mostprolific site (179 footprints documented) suggests that the tetrapods lived amongst small alethopterid trees colonizing the abandoned floor of a seasonally active fixed-channel river and a similar dryland context is probable for the seven other sites. The dominance of amniotes in these dryland alluvial facies contrastsmarkedly with coeval wetland facies in the nearby Joggins Formation, where skeletal and trackway assemblages are amphibian-dominated. This may imply that amniotes were better adapted to seasonally dry settings and sheds new light on the community ecology of tetrapods during a key evolutionary phase.

AB - Newly discovered tetrapod trackways are reported from eight sites in the Lower Pennsylvanian Tynemouth Creek Formation of southern New Brunswick, Canada. By far the most abundant and well-preserved tracks comprise pentadactyl footprints of medium size (32–53 mm long) with slender digits and a narrow splay (mostly b55°). Digit lengths typically approximate a phalangeal formula of 23453 (manus) and 23454 (pes), but this may vary due to extramorphology. These tracks are referred to Pseudobradypus and they are attributed to early amniotes. A second type of track (rare) comprises very small (5–8 mm long) tetradactyl manus, and incompletely preserved pedes. Referred to Batrachichnus, these are attributed to temnospondyl amphibians. A third type (also rare) comprises small pentadactyl pedes (20–25 mm long) showing stubby, widely splayed (152°) digits with a terminal bulge. Manus are probably pentadactyl (preservation incomplete) with a narrower digit splay. These footprints, classified as Baropezia, are attributed to anthracosaurs. Facies analysis at the mostprolific site (179 footprints documented) suggests that the tetrapods lived amongst small alethopterid trees colonizing the abandoned floor of a seasonally active fixed-channel river and a similar dryland context is probable for the seven other sites. The dominance of amniotes in these dryland alluvial facies contrastsmarkedly with coeval wetland facies in the nearby Joggins Formation, where skeletal and trackway assemblages are amphibian-dominated. This may imply that amniotes were better adapted to seasonally dry settings and sheds new light on the community ecology of tetrapods during a key evolutionary phase.

U2 - 10.1016/j.palaeo.2010.06.020

DO - 10.1016/j.palaeo.2010.06.020

M3 - Journal article

VL - 296

SP - 1

EP - 13

JO - Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences

JF - Palaeogeography, Palaeoclimatology, Palaeoecology - An International Journal for the Geo-Sciences

SN - 0031-0182

IS - 1-2

ER -

ID: 22336119