Crato Formation
Crato Formation | |
---|---|
Stratigraphic range: Latest Aptian ~ | |
Type | Geological formation |
Unit of | Santana Group |
Sub-units | Nova Olinda Member |
Underlies | Romualdo & Ipubi Formations |
Overlies | Barbalha Formation |
Lithology | |
Primary | Mudstone, limestone |
Other | Siltstone |
Location | |
Coordinates | 7°06′S 39°42′W / 7.1°S 39.7°W |
Approximate paleocoordinates | 8°36′S 8°00′W / 8.6°S 8.0°W |
Region | Ceará, Pernambuco |
Country | Brazil |
Extent | Araripe Basin |
Type section | |
Named for | Crato, Ceará |
Extent of the Santana Group, to which the Crato Formation belongs, in blue |
The Crato Formation is a geologic formation of Early Cretaceous (Aptian) age in northeastern Brazil's Araripe Basin. It is an important Lagerstätte (undisturbed fossil accumulation) for palaeontologists. The strata were laid down mostly during the Aptian age, about 113 million years ago. It thought to have been deposited in a semi-arid lacustrine wetland environment.[1]
The Crato Formation earns the designation of Lagerstätte due to an exceedingly well preserved and diverse fossil faunal assemblage. Some 25 species of fossil fishes are often found with stomach contents preserved, enabling paleontologists to study predator-prey relationships in this ecosystem. There are also fine examples of pterosaurs, reptiles and amphibians, invertebrates (particularly insects), and plants. Even dinosaurs are represented: a new maniraptor was described in 1996. The unusual taphonomy of the site resulted in limestone accretions that formed nodules around dead organisms, preserving even soft parts of their anatomy.
History
[edit]Fish fossils in the area were noted in 1823. When they were first methodically published, in 1993, the Crato Formation limestones provided a new site for pterosaurs, one that also preserved insects that fell into a brackish lagoon and semionotid fish preserved in phosphatized nodules. The fossils are usually compacted and preserved in layers of limestone. Fossil Odonata (dragonflies) and damselflies are especially rich in the Crato lagerstätte: currently 384 specimens have been recovered, 264 adults and 120 larvae. Hemiptera (true bugs) and Orthoptera (grasshoppers and crickets) are also abundant in number of species and in number of specimens. There are also plant remains.
Local mining activities for cement and construction damage the sites. Trade in illegally collected fossils has sprung up in the last decade, driven by the remarkable state of preservation and beauty of these fossils and amounting to a considerable local industry. An urgent preservation program is being called for by paleontologists.
In addition, the weathering of Crato and Santana Formation rocks has contributed soil conditions unlike elsewhere in the region. The Araripe manakin (Antilophia bokermanni) is a very rare bird that was discovered only in the late 20th century; it is not known from anywhere outside the characteristic forest that grows on the Chapada do Araripe soils formed ultimately from Crato and Santana Formation rocks.
Definition
[edit]The Crato Formation has often historically been considered the lowest member of the Santana Formation (or, alternatively, the Araripina Formation) of the Araripe Group,[2] later redefined as the Romualdo Formation of the Santana Group.[3][4] The Crato Member is the product of a single phase, where complicated sequence of sediment strata reflect changeable conditions in the opening sea. The age of this strata has been controversial, though most workers have agreed that it lies on or near the Aptian-Albian boundary, about 112 million years ago.[5]
The extent of the Crato unit and its relationship to the Romualdo Formation had long been ill-defined. It was not until a 2007 volume on the unit by Martill, Bechly and Loveridge that the Crato Formation was given a formal type locality, and was formally made a distinct formation separate from the Santana, which is about 10 Ma younger.[5] The Crato Formation is considered time equivalent with the Paracuru Formation.[6]
Fossil content
[edit]Insects
[edit](Note: Many more insects have been described than are present in the table below)
Inects of the Crato Formation | ||||
---|---|---|---|---|
Genus | Species | Presence | Description | Images |
A. seldoni |
Nova Olinda Member |
A Cratosmylidae lacewing[8] |
||
G. pulchra |
An Eolepidopterigidae moth |
|||
M. adamsi |
A Kalligrammatid lacewing |
|||
M. longimanus |
A Coxoplectopteran insect |
|||
N. nana |
An Eolepidopterigidae moth |
|||
P. incerta |
An Ithonidae lacewing, type species of Principiala |
|||
P. calipsa |
An Eolepidopterigidae moth |
|||
R. maxima |
||||
U. cariensis |
An Eolepidopterigidae moth |
|||
Astraeoptera[11] | A. vitrea | An Astraeopteridae mayfly. | ||
A. cretacica | ||||
A. oligovenata | ||||
Eosophobia[11] | E. acuta | An Astraeopteridae mayfly. |
Arachnids
[edit]Arachnids of the Crato Formation | ||||
---|---|---|---|---|
Genus | Species | Presence | Description | Images |
Mesoproctus[12] | M. rayoli | Whip Scorpion | ||
Protoischnurus | P. axelrodorum | Scorpion | ||
Cratosolpuga | C. wunderlichi | Solifuge |
Fish
[edit]Fish of the Crato Formation | |||||
---|---|---|---|---|---|
Genus | Species | Presence | Description | Images | Notes |
Araripelepidotes | Araripelepidotes temnurus | ||||
Belonostomus | Belonostomus sp. | ||||
Calamopleurus | Calamopleurus cylindricus | ||||
Cladocyclus | Cladocyclus gardneri | An Ichthyodectidae fish | |||
Cratoamia | Cratoamia gondwanica | ||||
Dastilbe | Dastilbe crandalli | ||||
Lepidotes | Lepidotes wenzae | ||||
Placidichthys | Placidichthys bidorsalis | ||||
Santanichthys | Santanichthys diasii |
Amphibians
[edit]Amphibians of the Crato Formation | ||||
---|---|---|---|---|
Genus | Species | Presence | Description | Images |
Arariphrynus placidoi[22] |
||||
Cratia gracilis[22] |
||||
Cratopipa novaolindensis |
||||
Eurycephalella alcinae[22] |
||||
Kururubatrachus gondwanicus |
||||
Possible indeterminate pipoid remains.[22] |
Squamata
[edit]Squamates of the Crato Formation | ||||
---|---|---|---|---|
Genus | Species | Presence | Description | Images |
C. alamoi |
A non-iguana lizard |
|||
T. amplectus |
A stem group snake with limbs |
Dinosaurs
[edit]Dinosaurs of the Crato Formation | ||||
---|---|---|---|---|
Genus | Species | Presence | Notes | Images |
?Avialan species |
Numerous isolated feathers |
|||
C. cearensis |
||||
K. mater |
||||
?Spinosaur species |
Isolated tooth listed in a book appendix.[5] It has later been suggested that the lithostratigraphic provenance of this specimen might have been incorrect.[26] |
|||
"U. jubatus" |
An informally-named compsognathid known from a partial skeleton preserving integument |
|||
Sauropoda footprints.[27] |
Crocodylomorphs
[edit]Crocodylomorphs of the Crato Formation | ||||
---|---|---|---|---|
Genus | Species | Presence | Description | Images |
Susisuchus anatoceps[28] |
||||
cf. Susisuchus sp.[29] |
Undescribed species |
Pterosaurs
[edit]Pterosaurs of the Crato Formation | ||||
---|---|---|---|---|
Genus | Species | Presence | Description | Images |
A. conandoylei |
||||
A. cearensis |
A basal member of the Tapejarinae. | |||
B. sp. |
||||
L. magnificens |
Nova Olinda Member |
|||
L. sibbicki |
An anhanguerid |
|||
T. imperator |
||||
?T. sp. |
Flora
[edit]Other fossils
[edit]- Araripenaeus timidus[31]
- †Cratoalloneura
- †Cratoatractocerus
- †Cratoborellia
- †Cratochrysa
- †Cratocora
- †Cratocordulia
- †Cratocoris
- †Cratocorydalopsis
- †Cratocossus
- †Cratodactylus
- †Cratoelcana
- †Cratoenigma
- †Cratogomphus
- †Cratogryllus
- †Cratohagenius
- †Cratohaglopsis
- †Cratohexagenites
- †Cratokalotermes
- †Cratolindenia
- †Cratolocustopsis
- †Cratolocustopsis araripensis
- †Cratolocustopsis contumax' – type locality for species
- †Cratolocustopsis cretacea
- †Cratomacer
- †Cratomastotermes
- †Cratomyia
- †Cratonemonyx
- †Cratonemopteryx
- †Cratonepa
- †Cratonerthra
- †Cratoneura
- †Cratonympha
- †Cratopelocoris
- †Cratopetalia
- †Cratopetalura
- †Cratopsychopsis
- †Cratopteryx
- †Cratoraricrus
- †Cratoscalapha
- †Cratosirex
- †Cratosisyrops
- †Cratosmylus
- †Cratostenophlebia
- †Cratotabanus
- †Cratotetraspinus
- †Cratotipula
- †Cratovitisma
- †Cratovoluptia
- †Cratozeunerella
See also
[edit]References
[edit]- ^ Ribeiro et al., 2021
- ^ Scherer et al., 2013, p. 28. Retrieved 2018-10-05.
- ^ Assine, 1992, p. 291. Retrieved 2018-10-05.
- ^ Fabin et al., 2018, p. 2050. Retrieved 2018-10-05.
- ^ a b c Martill et al., 2007. Retrieved 2018-10-06.
- ^ Leite da Silva, 2003. Retrieved 2018-10-06.
- ^ Myskowiak, 2016
- ^ Makarkin, Vladimir N.; Heads, Sam W.; Wedmann, Sonja (October 2017). "Taxonomic study of the Cretaceous lacewing family Babinskaiidae (Neuroptera: Myrmeleontoidea: Nymphidoidae), with description of new taxa". Cretaceous Research. 78: 149–160. doi:10.1016/j.cretres.2017.06.007. ISSN 0195-6671.
- ^ Bechly et al., 2016. Retrieved 2018-10-06.
- ^ Makarkin & Menon, 2007. Retrieved 2018-10-06.
- ^ a b Storari, Arianny P.; Staniczek, Arnold H.; Godunko, Roman J. (2023-07-20). "A new Gondwanan mayfly family from the Lower Cretaceous Crato Formation, Brazil (Ephemeroptera: Siphlonuroidea: Astraeopteridae fam. nov.)". Scientific Reports. 13 (1): 11735. Bibcode:2023NatSR..1311735S. doi:10.1038/s41598-023-36778-x. ISSN 2045-2322. PMC 10359310. PMID 37474555.
- ^ Santana, W.; Pinheiro, A. P.; Silva, T. A.; Lima, D. (2024). "Description of a new fossil Thelyphonida (Arachnida, Uropygi) and further record of Cratosolpuga wunderlichi Selden, in Selden and Shear, 1996 (Arachnida, Solifugae) from Crato Formation (Aptian/Albian), Araripe Basin, Brazil". PeerJ. 12. e16670. doi:10.7717/peerj.16670. PMC 10771091. PMID 38188171.
- ^ Aparecida et al., 2015, p. 25
- ^ Aparecida et al., 2015, p. 35
- ^ Aparecida et al., 2015, p. 29
- ^ Aparecida et al., 2015, p. 36
- ^ Aparecida et al., 2015, p. 31
- ^ Aparecida et al., 2015, p. 51
- ^ Aparecida et al., 2015, p. 26
- ^ Aparecida et al., 2015, p. 33
- ^ Aparecida et al., 2015, p. 47
- ^ a b c d e f g h Báez et al., 2009. Retrieved 2018-10-06.
- ^ Ismar de Souza Carvalho; Federico Agnolin; Mauro A. Aranciaga Rolando; Fernando E. Novas; José Xavier-Neto; Francisco Idalécio de Freitas; José Artur Ferreira Gomes de Andrade (2019). "A new genus of pipimorph frog (Anura) from the Early Cretaceous Crato formation (Aptian) and the evolution of South American tongueless frogs". Journal of South American Earth Sciences. 92: 222–233. Bibcode:2019JSAES..92..222C. doi:10.1016/j.jsames.2019.03.005. hdl:11336/123956. S2CID 134070810.
- ^ Federico Agnolin; Ismar Souza Carvalho; Alexis M. Aranciaga Rolando; Fernando E. Novas; José Xavier-Neto; José Artur Ferreira Gomes Andrade; Francisco Idalécio Freitas (2020). "Early Cretaceous neobatrachian frog (Anura) from Brazil sheds light on the origin of modern anurans". Journal of South American Earth Sciences. 101: Article 102633. Bibcode:2020JSAES.10102633A. doi:10.1016/j.jsames.2020.102633. S2CID 218957427.
- ^ de Souza Carvalho et al., 2021
- ^ Caetano, João Marcus Vale; Delcourt, Rafael & Ponciano, Luiza Corral Martins de Oliveira (March 2023). "A taxon with no name: Ubirajara jubatus (Saurischia: Compsognathidae) is an unavailable name and has no nomenclatural relevance". Zootaxa. 5254 (3): 443–446. doi:10.11646/zootaxa.5254.3.10. PMID 37044710.
- ^ Ismar de Souza, Carvalho Vale; Leonardi, Giuseppe; Rios-Netto, Aristoteles de Moraes; Borghi, Leonardo; Freitas, Alexandre de Paula; Andrade, José Artur & Freitas, Francisco Idalécio (2021). "Dinosaur trampling from the Aptian of Araripe Basin, NE Brazil, as tools for paleoenvironmental interpretation". Cretaceous Research. 117: 104626. Bibcode:2021CrRes.11704626C. doi:10.1016/j.cretres.2020.104626.
- ^ Salisbury et al., 2003. Retrieved 2018-10-06.
- ^ Figueiredo & Kellner, 2009. Retrieved 2018-10-06.
- ^ Jorge de Lima et al., 2015, p.102
- ^ Pinheiro, 2014, p. 4. Retrieved 2018-10-06.
Bibliography
[edit]- Aparecida dos Reis Polck, Márcia; Sardenberg Salgado de Carvalho, Marise; Miguel, Raphael; Gallo, Valéria (2015). Guia de identificação de peixes fósseis das Formações Crato e Santana da Bacia do Araripe. Serviço Geológico do Brasil (CPRM). pp. 1–74.
- Assine, Mario L (1992). "Análise estratigráfica da Bacia do Araripe, Nordeste do Brasil" (PDF). Revista Brasileira de Geociências. 22 (3): 289–300. doi:10.25249/0375-7536.1992289300.
- Báez, A.M.; Moura, G.J.B.; Gómez, R.O. (2009). "Anurans from the Lower Cretaceous Crato Formation of northeastern Brazil: implications for the early divergence of neobatrachians". Cretaceous Research. 30 (4): 829–846. Bibcode:2009CrRes..30..829B. doi:10.1016/j.cretres.2009.01.002.
- Bechly, G.; Makarkin, V. N. (2016). "A new gigantic lacewing species (Insecta: Neuroptera) from the Lower Cretaceous of Brazil confirms the occurrence of Kalligrammatidae in the Americas". Cretaceous Research. 58: 135–140. Bibcode:2016CrRes..58..135B. doi:10.1016/j.cretres.2015.10.014.
- de Souza Carvalho, I.; Agnolin, F. L.; Rozadilla, S.; Novas, F. E.; Ferreira Gomes Andrade, J. A.; Xavier-Neto, J. (2021). "A new ornithuromorph bird from the Lower Cretaceous of South America". Journal of Vertebrate Paleontology. 41 (4): e1988623. Bibcode:2021JVPal..41E8623C. doi:10.1080/02724634.2021.1988623. S2CID 244059488. S2CID 244059488
- Fabin, Carlos E.; Correia Filho, Osvaldo J.; Alencar, Márcio L.; Barbosa, José A.; de Miranda, Tiago S.; Neumann, Virgínio H.; Gomes, Igor F.; de Santana, Felipe R. (2018). "Stratigraphic Relations of the Ipubi Formation: Siliciclastic-Evaporitic Succession of the Araripe Basin" (PDF). Anais da Academia Brasileira de Ciências. 90 (2 suppl 1): 2049–2071. doi:10.1590/0001-3765201820170526. PMID 29947671.
- Figueiredo, R.G.; Kellner, A.W.A. (2009). "A new crocodylomorph specimen from the Araripe Basin (Crato Member, Santana Formation), northeastern Brazil". Paläontologische Zeitschrift. 83 (2): 323–331. Bibcode:2009PalZ...83..323F. doi:10.1007/s12542-009-0016-6. S2CID 129166567.
- Jorge de Lima, Flaviana; Feitosa Saraiva, Antonio Álamo; Manso Sayão, Juliana (2012). "Revisão da paleoflora das Formações Missão Velha, Crato e Romualdo, Bacia do Araripe, nordeste do Brasil". Estudos Geológicos. 22 (1): 99–115. doi:10.18190/1980-8208/estudosgeologicos.v22n1p99-115.
- Leite da Silva, Agnelo; Neumann, Virginio Enrique (2003). Formação Crato da Bacia do Araripe: um reservatório análogo ao Calcário Trairí (Formação Paracuru), Bacia do Ceará (PDF). 2o Congresso Brasileiro de P&D em Petróleo & Gás. pp. 1–6.
- Makarkin, V.N.; Menon, F. (2007). "First record of fossil 'rapismatid-like' Ithonidae (Insecta, Neuroptera) from the Lower Cretaceous Crato Formation of Brazil". Cretaceous Research. 28 (5): 743–753. Bibcode:2007CrRes..28..743M. doi:10.1016/j.cretres.2006.11.003.
- Martill, David M.; Bechly, Günter; Loveridge, Robert F. (2007). The Crato Fossil Beds of Brazil: Window into an Ancient World. Cambridge University Press. p. 236. ISBN 978-1-139-46776-6.
- Pinheiro, Allysson P.; Saraiva, Antônio Á.F.; Santana, William (2014). "Shrimps from the Santana Group (Cretaceous: Albian): new species (Crustacea: Decapoda: Dendrobranchiata) and new record (Crustacea: Decapoda: Caridea)" (PDF). Anais da Academia Brasileira de Ciências. 86 (2): 1–8. doi:10.1590/0001-3765201420130338. PMID 24789213. Archived from the original (PDF) on 2017-08-24.
- Ribeiro, Alexandre Cunha; Ribeiro, Guilherme Cunha; Varejão, Filipe Giovanini; Battirola, Leandro Dênis; Pessoa, Edlley Max; Simões, Marcello Guimarães; Warren, Lucas Veríssimo; Riccomini, Claudio; Poyato-Ariza, Francisco José (May 2021). "Towards an actualistic view of the Crato Konservat-Lagerstätte paleoenvironment: A new hypothesis as an Early Cretaceous (Aptian) equatorial and semi-arid wetland". Earth-Science Reviews. 216: 103573. Bibcode:2021ESRv..21603573R. doi:10.1016/j.earscirev.2021.103573. S2CID 233924513.
- Salisbury, S.W.; Frey, E.; Martill, D.M.; Buchy, M.C. (2003). "A new crocodilian from the Lower Cretaceous Crato Formation of north-eastern Brazil". Palaeontographica, Abteilung A. 270 (1–3): 3–47. Bibcode:2003PalAA.270....3S. doi:10.1127/pala/270/2003/3. S2CID 128437299.
- Scherer, C.M.d.S.; Jardim de Sá, E.F.; Córdoba, V.C.; Sousa, D.d.C.; Aquino, M.M.; Cardoso, F.M.C. (2013). "Tectono-Stratigraphic evolution of the upper Jurassic-Neocomian rift succession, Araripe Basin, Northeast Brazil" (PDF). Journal of South American Geosciences. 49: 1–43. Bibcode:2014JSAES..49..106M. doi:10.1016/j.jsames.2013.10.007. hdl:10316/27124.
- Weishampel, David B.; et al. (2004). Dinosaur distribution (Early Cretaceous, South America) in: Weishampel, David B.; Dodson, Peter; and Osmólska, Halszka (eds.): The Dinosauria. Berkeley: University of California Press. pp. 563–570. ISBN 0-520-24209-2.
Further reading
[edit]- Bétard, François; Peulvast, Jean-Pierre; de Oliveira Magalhães, Alexsandra; Carvalho Neta, Maria de Lourdes; de Freitas, Francisco Idalecio (2017). "Araripe Basin: A Major Geodiversity Hotspot in Brazil" (PDF). Geoheritage. 10 (4): 1–18. Bibcode:2018Geohe..10..543B. doi:10.1007/s12371-017-0232-5. Archived from the original (PDF) on 2018-08-21.
- Neumann, V.H.; Borrego, A.G.; Cabrera, L.; Dino, R. (2003). "Organic matter composition and distribution through the Aptian–Albian lacustrine sequences of the Araripe Basin, northeastern Brazil". International Journal of Coal Geology. 54 (1): 21–40. Bibcode:2003IJCG...54...21N. doi:10.1016/S0166-5162(03)00018-1.
- Jouault, C.; Nel, A. (2020). "The first fossil horntail wasp (Hymenoptera: Siricidae) from Lower Cretaceous Crato Formation in Brazil". Palaeoentomology. 003: 382–389. doi:10.11646/palaeoentomology.3.4.10. S2CID 225217001.
- Nel, A.; Pouillon, J-M. (2020). "The second genus of the 'libelluloid' family Araripephlebiidae (Odonata, Clavilabiata)". Palaeoentomology. 003: 240–244. doi:10.11646/palaeoentomology.3.3.4. S2CID 225751809.
- Crato Formation
- Geologic formations of Brazil
- Lower Cretaceous Series of South America
- Cretaceous Brazil
- Mudstone formations
- Limestone formations
- Deltaic deposits
- Lacustrine deposits
- Paleontology in Brazil
- Environment of Ceará
- Environment of Pernambuco
- Environment of Piauí
- Landforms of Ceará
- Landforms of Pernambuco
- Landforms of Piauí
- Northeast Region, Brazil