User:Yewtharaptor/sandbox
| Port des Canonge Formation | |
|---|---|
| Stratigraphic range: Early-Middle? Permian, | |
 Exposed redbeds | |
| Type | Geological formation |
| Underlies | Pedra de s'Ase Formation |
| Overlies | Bec de s'Àguila Formation |
| Lithology | |
| Primary | sandstone, mudstone, lutite |
| Location | |
| Coordinates | 39.7° N, 2.6° E |
| Region |  Mallorca |
| Country |  Spain |
| Type section | |
| Named for | Port d'es Canonge village |
The Port des Canonge Formation is an Early-Middle Permian-age geologic formation in the Mediterranean island of Mallorca. It consists of red to brown-colored sedimentary rocks (red beds) such as sandstone and mudstone, and is located in what back then was the western peri-Tethys Ocean.[1]
Geological Context
[edit]
The Permian geological context of Mallorca is part of the larger framework of the Balearic Islands, an extension of the Betic fold and thrust belt formed during the Alpine orogeny. On the islands, only Mallorca and Menorca have exposed Permian beds, likely derived from sedimentary successions deposited in isolated basins along the eastern edge of the Iberian plate, sharing a structural connection with the Iberian Peninsula, emerged during the collapse of the Variscan orogeny in the Late Carboniferous to Early Permian. This collapse led to a transtensional and extensional tectonic regime, creating semi-graben structures that facilitated sediment accumulation.[2][3]
Palaeogeographically, these basins were located in the western peri-Tethys and shifted from approximately 7°S to 4°N latitude throughout the Permian, experiencing a tropical, semi-arid, and seasonal climate.[2] On Mallorca, Permian rocks are primarily found along the coastal cliffs of the Serra de Tramuntana and partially inland, though often obscured by forest cover. The base of the Permian succession is faulted against underlying Carboniferous rocks, and the transition to the overlying Lower Triassic Buntsandstein is marked by an unconformity, identified for the first time in this study.[1][2]
Paleoenvironment
[edit]
The Port des Canonge Formation represents a intra-continental fine-grained meandering river system with extensive floodplain deposits, flowing southeast along the basin’s main axis. It is composed of red sandstones and red lutites organized in fining-upward sequences, dominated by lateral accretion surfaces from channel bars and overbank deposits. Breccia lithofacies occur as basal lags or isolated beds, reflecting reworked floodplain sediments. Sandstone lithofacies include ripple-marked, laminated, and massive sands, indicating waning flows and overbank deposits. Floodplain lutites are characterized by massive and laminated facies, disrupted by plant roots and invertebrate burrows during periods of low sedimentation or subaerial exposure.[1][4] Decreased subsidence rates favored a longitudinal fluvial system, while significant accommodation space allowed for the deposition of mudstones and fine sandstones.[4]
The system is marked by lateral accretion surfaces and stabilized riverbanks, likely due to abundant floodplain vegetation, which prevented channel widening. Evidence of this vegetation includes developed soils, occasional plant remains, and logs despite the oxidized conditions.[1]
Palaeosols with carbonate nodules, calcrete hardpans, and gleyed patches developed under dry conditions, pointing to seasonal desiccation of ponds, which likely functioned as waterholes. Fossils, including tetrapod tracks and skeletons, rhizocretions, and plant remains, emphasize the ecological importance of these floodplain environments.[1][4]
The formation’s palaeocurrents suggest a southeast-directed flow, consistent with the meandering river interpretation. Overall, the facies suggest a semi-arid, dynamic fluvial system shaped by meandering rivers & seasonal dry periods.[1][4]
Paleobiota
[edit]Color key
|
Notes Uncertain or tentative taxa are in small text; |
Invertebrates
[edit]| Genus | Species | Location | Material | Made by | Images |
|---|---|---|---|---|---|
| Arenicolites[1] |
|
Port des Canonge–Hort de sa Cova | Burrowing Traces |
|
 |
| Cochlichnus[1] |
|
Torrent de na Nadala | Burrows |
|
|
| Cruziana[1] |
|
Port des Canonge–Hort de sa Cova | Feeding trace | ||
| Palaeophycus[1] |
|
Port des Canonge–Hort de sa Cova | Burrows |  | |
| Planolites[1] |
|
Port des Canonge–Hort de sa Cova | Burrows |
|
 |
Amniotes
[edit]| Genus | Species | Location | Material | Notes | Images |
|---|---|---|---|---|---|
| Characichnos[1] |
|
Torrent de na Nadala
Racó de s'Algar |
Footprints | Swimming tetrapod tracks | |
| Dimetropus[1] |
|
Torrent de na Nadala | Footprints | Tetrapod tracks, referred to multiple early synapsids: caseidae, ophiacodontidae, edaphosauridae and sphenacodontidae |  |
| Dromopus[1] |
|
Torrent de na Nadala | Footprints | Tetrapod tracks, referred to Araeoscelidians or Varanopidae | |
| Gorgonopsia[4] | Indeterminate | Torrent de na Nadala | DA21/17-01-01, disarticulated partial skeleton | A relatively small Gorgonopsian therapsid, representing the oldest record of the group worldwide | |
| Hyloidichnus[1] |
|
Torrent de na Nadala | Footprints | Tetrapod tracks, referred to Captorhinomorpha eureptiles |  |
| Moradisaurinae[5] | Indeterminate | Cala Gata | MBCN 15730, a partial right maxilla and parts of the palate | A Captorhinidan eureptile | |
| Pachypes[1] |
|
Torrent de na Nadala | Footprints | Tetrapod tracks, referred to Pareiasauromorph parareptiles |
Plants
[edit]Multiple large logs along carbonaceous debris have been found in Cova des Carbó.[1]
| Genus | Species | Stratigraphic position | Material | Notes | Images |
|---|---|---|---|---|---|
| Hermitia[1] |
|
Torrent de na Nadala | Three foliated penultimate shoot fragments | Branched shoots referred to conifers, probably Voltziales | |
| Feysia[1] |
|
Torrent de na Nadala
Racó de s'Algar Platjola des munt de Pedres Es Tamarell |
Branched shoots | Branched shoots referred to conifers, probably Voltziales |
References
[edit]- ^ a b c d e f g h i j k l m n o p q r s Matamales-Andreu, Rafel; Mujal, Eudald; Dinarès-Turell, Jaume; Kustatscher, Evelyn; Roghi, Guido; Oms, Oriol; Galobart, Àngel; Fortuny, Josep (2022). "Early–middle Permian ecosystems of equatorial Pangaea: Integrated multi-stratigraphic and palaeontological review of the Permian of Mallorca (Balearic Islands, western Mediterranean)". Earth-Science Reviews. 228: 103948. doi:10.1016/j.earscirev.2022.103948. ISSN 0012-8252.
- ^ a b c López-Gómez, José; Alonso-Azcárate, Jacinto; Arche, Alfredo; Arribas, José; Fernández Barrenechea, José; Borruel-Abadía, Violeta; Bourquin, Sylvie; Cadenas, Patricia; Cuevas, Julia (2019), Quesada, Cecilio; Oliveira, José Tomás (eds.), "Permian-Triassic Rifting Stage", The Geology of Iberia: A Geodynamic Approach: Volume 3: The Alpine Cycle, Cham: Springer International Publishing, pp. 29–112, doi:10.1007/978-3-030-11295-0_3, ISBN 978-3-030-11295-0, retrieved 2024-12-17
- ^ Roscher, Marco; Schneider, Joerg W. (2006). "Permo-Carboniferous climate: Early Pennsylvanian to Late Permian climate development of central Europe in a regional and global context". Geological Society, London, Special Publications. 265 (1): 95–136. doi:10.1144/GSL.SP.2006.265.01.05.
- ^ a b c d e Matamales-Andreu, Rafel; Kammerer, Christian F.; Angielczyk, Kenneth D.; Simões, Tiago R.; Mujal, Eudald; Galobart, Àngel; Fortuny, Josep (2024-12-17). "Early–middle Permian Mediterranean gorgonopsian suggests an equatorial origin of therapsids". Nature Communications. 15 (1): 10346. doi:10.1038/s41467-024-54425-5. ISSN 2041-1723.
- ^ Liebrecht, Torsten; Fortuny, Josep; Galobart, Àngel; Müller, Johannes; Sander, P. Martin (2016-12-07). "A large, multiple-tooth-rowed captorhinid reptile (Amniota: Eureptilia) from the Upper Permian of Mallorca (Balearic Islands, western Mediterranean)". Journal of Vertebrate Paleontology. 37 (1): e1251936. doi:10.1080/02724634.2017.1251936. ISSN 0272-4634.