The La Quinta Formation is composed of three fossiliferous members, which are as follows, in stratigraphic order (lowest to highest):
Camino Carretero Member: This member, know to get up to 2,650ft (810m) in thickness, is primarily composed of various sandstones. Some of the sandstone layers are noted to be cemented with calcium carbonate, whilst non-calcareous sandstones layers range from brown-ochre to grey weather limoitic fine-grained, alternating massive to thin-bedded fine to coarse-grained brown weathering, coarse-grained arkosic, blue-grey to buff-micaceous fine-grained buff to brown weathering, and buff medium-grained micaceous buff to ochre weathering tuffaceous medium-grained with inter-bedded calcareous rocks. Towards the upper 800ft (240m) of the member, the various sandstones give way to tuffaceous sandstones, ranging from buff to limonitic or red tuffaceous sandstone, which is inter-bedded with siltstone, to massive silty medium-grained micaceous tuffaceous limonitic weathering sandstone. Throughout this member, shales are also present, starting as a blue-grey calcareous shale in the lower sections of the member, giving way to sandy shale, buff to micaceous-green shale, buff-micaceous silty ochre weathering shale, fissule limonitic shale, and reddish-brown fissile shale towards the middle sections, although almost become completely absent in the upper sections, save for a layer of dark-grey to black shale. Siltstones are also common within the lower sections of the member, ranging from sandy siltstone, buff to ochre-micaceous siltstone, tan siltstone with inter-bedded marly, tan to dark green-grey weathering siltstone to fine-grained sandstone, blue-grey to brown calcareous siltstone to fine-grained sandstone, tuffaceous massive grey limonitic weathering siltstone to medium-grained sandstone, and minor tuffaceous limonitic weathering sandy siltstones. Limestones can also be found, although it is notably uncommon, only being found as thin layers in the lower and upper sections of member.[3]
Florida Limestone Member: This member, known to get up to 150ft (46m) in thickness, is predominately composed of silty limestone, calcareous shale, sandy limestone. In other outcroppings, the member is also composed of algal limestone, lignitic limestone, and massive white limestone.[3]
Finca Carmitto Member: This member, which is roughly 100ft (30m) thick, is primarily composed of sandy pebble conglomerate in its lower section, whilst in the upper section it is composed of dark-grey to black rubbly shale and thin light buff-whitish weathering medium-grained calcareous sandstone, which is laminated in nature.[3]
Dating
Using U–Pb dating on zircon samples collected from around the upper amber bearing sections, the Mexican amber biota of the La Quinta Formation was constrained to between 24Ma and 20Ma.[1]
Paleobiota
The biota of the La Quinta Formation is primarily composed of various arthropods, from wasps such as Hyptia deansi,[4] to ostracods as Thalassocypria.[5] It is also home to a wide variety of plants, such as the fabacid Simojoflorum mijangosii.[6]
12Riquelme, Francisco; Ortega-Flores, Berlaine; Estrada-Ruiz, Emilio; Córdova-Tabares, Víctor (1 June 2025). "Zircon U–Pb ages of the Chiapas Amber-Lagerstätte in the uppermost Simojovel Formation, southwest Mexico". Canadian Journal of Earth Sciences. 62 (6): 1088–1103. doi:10.1139/cjes-2024-0100.
123456789101112131415161718192021222324Graham, Alan (January 1999). "Studies in Neotropical paleobotany. XIII. An Oligo‐Miocene palynoflora from Simojovel (Chiapas, Mexico)". American Journal of Botany. 86 (1): 17–31. doi:10.2307/2656951.
123Allison, R. C. (1967). The Cenozoic Stratigraphy of Chiapas, Mexico: With Discussions of the Classification of the Turritellidae and Selected Mexican Representatives. University of California. pp.1–553. ISBN9781085391153.
123456Matzke-Karasz, Renate; Serrano-Sánchez, María de Lourdes; Pérez, Liseth; Keyser, Dietmar; Pipík, Radovan; Vega, Francisco J. (7 February 2019). "Abundant assemblage of Ostracoda (Crustacea) in Mexican Miocene amber sheds light on the evolution of the brackish-water tribe Thalassocypridini". Historical Biology. 31 (2): 65–101. doi:10.1080/08912963.2017.1340471.
↑Poinar, G.; Doyen, J. T. (1992). "A fossil termite bug, Termitaradus protera sp. n. (Hemiptera: Termitaphididae), from Mexican amber". Entomologica Scandinavica. 23: 89–93. doi:10.1163/187631292X00047.
↑De Andrade, M. L. (1995). "The ant genus Aphaenogaster in Dominican and Mexican amber (Amber Collection Stuttgart: Hymenoptera, Formicidae. IX: Pheidolini)". Stuttgarter Beiträge zur Naturkunde. Serie B (Geologie und Paläontologie). 223: 1–11.
↑Conty, D; Garrouste, R; Nel, A (2014). "The first lace bug from Chiapas amber (Totolapa, Mexico) (Hemiptera: Tingidae)". Annales de la Société Entomologique de France. New Series. 50 (3–4): 286–290. doi:10.1080/00379271.2014.982024. S2CID83251915.–viaTaylor & Francis(subscription required)
↑Ojeda, Margarita; Vega, Francisco J.; Rivas, Gerardo (January 2023). "Ceratozetidae (Acari: Oribatida) from lower Miocene mexican amber, including a new species of Trichoribates". Journal of South American Earth Sciences. 121: 104165. doi:10.1016/j.jsames.2022.104165.{{cite journal}}: CS1 maint: article number as page number (link)
12Zheng, Daran; Nel, André; Jarzembowski, Edmund A.; Chang, Su-Chin; Zhang, Haichun; Wang, Bo (2 January 2019). "Exceptionally well-preserved dragonflies (Insecta: Odonata) in Mexican amber". Alcheringa: An Australasian Journal of Palaeontology. 43 (1): 157–164. doi:10.1080/03115518.2018.1456562.
↑Engel, Michael S. (13 May 2014). "An orchid bee of the genus Eulaema in Early Miocene Mexican amber (Hymenoptera: Apidae)". Novitates Paleoentomologicae (7): 1. doi:10.17161/np.v0i7.4726.
↑Poinar, George; Thomas, Donald B. (April 2012). "A stink bug, Edessa protera sp. n. (Pentatomidae: Edessinae) in Mexican amber". Historical Biology. 24 (2): 207–211. doi:10.1080/08912963.2011.602403.
1234567Huys, Rony; Suárez-Morales, Eduardo; Serrano-Sánchez, María de Lourdes; Centeno-García, Elena; Vega, Francisco J. (12 October 2016). "Early Miocene amber inclusions from Mexico reveal antiquity of mangrove-associated copepods". Scientific Reports. 6 (1). doi:10.1038/srep34872.
123Poinar, George O. (1977). "Fossil Nematodes From Mexican Amber". Nematologica. 23 (2): 232–238. doi:10.1163/187529277X00589.
123456789Frost, Stanley H.; Langenheim, Ralph L. (1974). Cenozoic reef biofacies: Tertiary larger Foraminifera and scleractinian corals from Chiapas, Mexico. DeKalb, Ill: Northern Illinois University Press. ISBN0875800270.
↑Hernández-Damián, Ana L.; Cevallos-Ferriz, Sergio R. S.; Huerta-Vergara, Alma R. (December 2017). "Fossil flower of Staphylea L. from the Miocene amber of Mexico: New evidence of the Boreotropical Flora in low-latitude North America". Earth and Environmental Science Transactions of the Royal Society of Edinburgh. 108 (4): 471–478. doi:10.1017/S1755691018000701.
↑Castañeda‐Posadas, Carlos; Cevallos‐Ferriz, Sergio R. S. (November 2007). "Swietenia (Meliaceae) flower in Late Oligocene–Early Miocene amber from Simojovel de Allende, Chiapas, Mexico". American Journal of Botany. 94 (11): 1821–1827. doi:10.3732/ajb.94.11.1821.
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