Crato Formation
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.
| 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 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
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
The Crato Formation has often historically been considered the lowest member of the Santana Formation (or, alternatively, the Araripina Formation) of the Araripe Group, later redefined as the Romualdo Formation of the Santana Group. 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.
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. The Crato Formation is considered time equivalent with the Paracuru Formation.
Fossil content
Insects
(Note: Many more insects have been described than are present in the table below)
| Insects of the Crato Formation | ||||
|---|---|---|---|---|
| Genus | Species | Presence | Description | Images |
| A. seldoni | Nova Olinda Member | A Nymphid lacewing | ||
| 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 | |||
| Rafaeliana | R. maxima | |||
| U. cariensis | An Eolepidopterigidae moth | |||
| Astraeoptera | A. vitrea | An Astraeopteridae mayfly. | ||
| A. cretacica | ||||
| A. oligovenata | ||||
| Eosophobia | E. acuta | An Astraeopteridae mayfly. | ||
Arachnids
| Arachnids of the Crato Formation | ||||
|---|---|---|---|---|
| Genus | Species | Presence | Description | Images |
| Protoischnurus | P. axelrodorum | Scorpion | ||
| Cratosolpuga | C. wunderlichi | Solifuge | ||
Fish
| 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
| Amphibians of the Crato Formation | ||||
|---|---|---|---|---|
| Genus | Species | Presence | Description | Images |
| Arariphrynus | Arariphrynus placidoi | |||
| Cratia gracilis | ||||
| Eurycephalella alcinae | ||||
| Possible indeterminate pipoid remains. | ||||
Squamata
| Squamatans of the Crato Formation | ||||
|---|---|---|---|---|
| Genus | Species | Presence | Description | Images |
| C. alamoi | A non-iguana lizard | |||
| T. amplectus | A stem group snake with limbs |  | ||
Dinosaurs
| 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. It has later been suggested that the lithostratigraphic provenance of this specimen might have been incorrect. | |||
| "U. jubatus" | An informally-named compsognathid known from a partial skeleton preserving integument |  | ||
| Sauropoda footprints. | ||||
Crocodylomorphs
| Crocodylomorphs of the Crato Formation | ||||
|---|---|---|---|---|
| Genus | Species | Presence | Description | Images |
| Susisuchus anatoceps |  | |||
| cf. Susisuchus sp. | Undescribed species | |||
Pterosaurs
| 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
| Flora of the Crato Formation | |
|---|---|
| Species | Notes |
| Araucaria cartellei, Brachyphyllum obesum, B. castilhoi, B. insigne, Iara iguassu, Caytoniales sp., Ephedra sp., Araripia florifera, Araucarites vulcanoi, Cariria orbiculiconiformis, Cearania heterophylla, Cratonia cotyledon, Endressinia brasiliana,Klitzchophyllites flabellatus, Novaolindia dubia, Pluricarpellatia peltata, Podozamites lanceolatus, Protananas lucenae, Ruffordia goeppertii, Tomaxellia biforme, Welwitschiaprisca austroamericana, Welwitschiophyllum brasiliense, Welwitschiostrobus murili, Araucariostrobus sp., Frenelopsis sp., Isoetites sp., Lindleycladus sp., Schizoneura sp. | |
Other fossils
- Araripenaeus timidus
- †Cratoalloneura
- †Cratoalloneura acuminata
- †Cratoalloneura verdandia
- †Cratoatractocerus
- †Cratoatractocerus grimaldii
- †Cratoborellia
- †Cratoborellia gorbi
- †Cratochrysa
- †Cratochrysa martinsnetoi
- †Cratochrysa sublapsa
- †Cratochrysa willmanni
- †Cratocora
- †Cratocora crassa
- †Cratocordulia
- †Cratocordulia borschukewitzi
- †Cratocoris
- †Cratocoris shevchenkoae
- †Cratocorydalopsis
- †Cratocorydalopsis brasiliensis
- †Cratocossus
- †Cratocossus magnus
- †Cratodactylus
- †Cratodactylus ferreirai
- †Cratodactylus kellneri
- †Cratoelcana
- †Cratoelcana damianii
- †Cratoelcana zessini
- †Cratoenigma
- †Cratoenigma articulata
- †Cratogomphus
- †Cratogomphus erraticus
- †Cratogryllus
- †Cratogryllus cigueli
- †Cratogryllus guimaraesae
- †Cratogryllus pentagonalis
- †Cratohagenius
- †Cratohagenius erichweberi
- †Cratohaglopsis
- †Cratohaglopsis santanaensis
- †Cratohexagenites
- †Cratohexagenites longicercus
- †Cratohexagenites minor
- †Cratokalotermes
- †Cratokalotermes santanensis
- †Cratolindenia
- †Cratolindenia knuepfae
- †Cratolocustopsis
- †Cratolocustopsis araripensis
- †Cratolocustopsis contumax' – type locality for species
- †Cratolocustopsis cretacea
- †Cratomacer
- †Cratomacer ephippiger
- †Cratomacer immersus
- †Cratomastotermes
- †Cratomastotermes wolfschwenningeri
- †Cratomyia
- †Cratomyia cretacica
- †Cratomyia macrorrhyncha
- †Cratonemonyx
- †Cratonemonyx martinsnetoi
- †Cratonemopteryx
- †Cratonemopteryx audax
- †Cratonemopteryx robusta
- †Cratonemopteryx speciosa
- †Cratonepa
- †Cratonepa enigmatica
- †Cratonerthra
- †Cratonerthra corinthiana
- †Cratonerthra estevezae
- †Cratoneura
- †Cratoneura dividens
- †Cratoneura longissima
- †Cratoneura pulchella
- †Cratonympha
- †Cratonympha microcelata
- †Cratopelocoris
- †Cratopelocoris carpinteroi
- †Cratopetalia
- †Cratopetalia whiteheadi
- †Cratopetalura
- †Cratopetalura petruleviciusi
- †Cratopetalura petruleviciusi
- †Cratopsychopsis
- †Cratopsychopsis maiseyi
- †Cratopteryx
- †Cratopteryx nemopteroides
- †Cratopteryx robertosantosi
- †Cratoraricrus
- †Cratoraricrus oberlii
- †Cratoscalapha
- †Cratoscalapha electroneura
- †Cratosirex
- †Cratosirex sennlaubi
- †Cratosisyrops
- †Cratosisyrops gonzagai
- †Cratosmylus
- †Cratosmylus magnificus
- †Cratostenophlebia
- †Cratostenophlebia schwickerti
- †Cratotabanus
- †Cratotabanus stonemyomorphus
- †Cratotetraspinus
- †Cratotetraspinus fossorius
- †Cratotipula
- †Cratotipula latialata
- †Cratovitisma
- †Cratovitisma oldreadi
- †Cratovoluptia
- †Cratovoluptia criptoneura
- †Cratozeunerella
- †Cratozeunerella amedegnatoi
- †Cratozeunerella godoii
- †Cratozeunerella neotropica
- †Cratozeunerella nervosa
- †Cratozeunerella soaresi
- †Cratozeunerella titanella
See also
References
- 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.
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