A Several-Kilometer-Long Archosaur Route in the Triassic of the Swiss Alps

The Mesozoic sedimentary cover of the Aiguilles Rouges Massif straddling the Swiss-French border has yielded several archosaur footprint sites dated to the Early or Middle Triassic and composed of mostly poorly preserved footprints lacking any orderly arrangement and resting on a megatracksite level...

Full description

Bibliographic Details
Main Authors: Lionel Cavin, André Piuz
Format: Article
Language:English
Published: Frontiers Media S.A. 2020-02-01
Series:Frontiers in Earth Science
Subjects:
Online Access:https://www.frontiersin.org/article/10.3389/feart.2020.00004/full
id doaj-78868c89b72a4a9384f19cf02b12a1af
record_format Article
spelling doaj-78868c89b72a4a9384f19cf02b12a1af2020-11-24T22:26:29ZengFrontiers Media S.A.Frontiers in Earth Science2296-64632020-02-01810.3389/feart.2020.00004508500A Several-Kilometer-Long Archosaur Route in the Triassic of the Swiss AlpsLionel CavinAndré PiuzThe Mesozoic sedimentary cover of the Aiguilles Rouges Massif straddling the Swiss-French border has yielded several archosaur footprint sites dated to the Early or Middle Triassic and composed of mostly poorly preserved footprints lacking any orderly arrangement and resting on a megatracksite level. Here we describe two short archosaur trackways attributed to Isochirotherium herculis and located at ca. 2400 m asl in two distinct small valleys separated from each other by a linear distance of 6.4 km. Projection of both trackways onto the same plane showed that they were aligned with a deviation angle of only 3°. These aligned trackways are interpreted as remnants of a straight and narrow walking route taken by a single trackmaker species. It is possible that both trackway segments were made by the same individual. In the present landscape, the Triassic outcrops are small and scattered along a roughly straight NE-SW line. The orientation of the trackways agrees with the general orientation of the outcrops, which is very unlikely to be caused by chance only. We explain this apparent coincidence as resulting from the structural inheritance of a general NE-SW Paleozoic shear zone that controlled the orientation of the Vindelician High on which the archosaurs walked, then that defined the axis of the much later Massif uplift, and eventually affected the general orientation of the erosion that uncovered the trackways.https://www.frontiersin.org/article/10.3389/feart.2020.00004/fullpaleoichnologyethologyorogenyTriassicChirotheriidaefootprint
collection DOAJ
language English
format Article
sources DOAJ
author Lionel Cavin
André Piuz
spellingShingle Lionel Cavin
André Piuz
A Several-Kilometer-Long Archosaur Route in the Triassic of the Swiss Alps
Frontiers in Earth Science
paleoichnology
ethology
orogeny
Triassic
Chirotheriidae
footprint
author_facet Lionel Cavin
André Piuz
author_sort Lionel Cavin
title A Several-Kilometer-Long Archosaur Route in the Triassic of the Swiss Alps
title_short A Several-Kilometer-Long Archosaur Route in the Triassic of the Swiss Alps
title_full A Several-Kilometer-Long Archosaur Route in the Triassic of the Swiss Alps
title_fullStr A Several-Kilometer-Long Archosaur Route in the Triassic of the Swiss Alps
title_full_unstemmed A Several-Kilometer-Long Archosaur Route in the Triassic of the Swiss Alps
title_sort several-kilometer-long archosaur route in the triassic of the swiss alps
publisher Frontiers Media S.A.
series Frontiers in Earth Science
issn 2296-6463
publishDate 2020-02-01
description The Mesozoic sedimentary cover of the Aiguilles Rouges Massif straddling the Swiss-French border has yielded several archosaur footprint sites dated to the Early or Middle Triassic and composed of mostly poorly preserved footprints lacking any orderly arrangement and resting on a megatracksite level. Here we describe two short archosaur trackways attributed to Isochirotherium herculis and located at ca. 2400 m asl in two distinct small valleys separated from each other by a linear distance of 6.4 km. Projection of both trackways onto the same plane showed that they were aligned with a deviation angle of only 3°. These aligned trackways are interpreted as remnants of a straight and narrow walking route taken by a single trackmaker species. It is possible that both trackway segments were made by the same individual. In the present landscape, the Triassic outcrops are small and scattered along a roughly straight NE-SW line. The orientation of the trackways agrees with the general orientation of the outcrops, which is very unlikely to be caused by chance only. We explain this apparent coincidence as resulting from the structural inheritance of a general NE-SW Paleozoic shear zone that controlled the orientation of the Vindelician High on which the archosaurs walked, then that defined the axis of the much later Massif uplift, and eventually affected the general orientation of the erosion that uncovered the trackways.
topic paleoichnology
ethology
orogeny
Triassic
Chirotheriidae
footprint
url https://www.frontiersin.org/article/10.3389/feart.2020.00004/full
work_keys_str_mv AT lionelcavin aseveralkilometerlongarchosaurrouteinthetriassicoftheswissalps
AT andrepiuz aseveralkilometerlongarchosaurrouteinthetriassicoftheswissalps
AT lionelcavin severalkilometerlongarchosaurrouteinthetriassicoftheswissalps
AT andrepiuz severalkilometerlongarchosaurrouteinthetriassicoftheswissalps
_version_ 1725753425218502656