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Paleobiota of the Posidonia Shale

Fossil flora and fauna in the Posidonia Shale, Germany From Wikipedia, the free encyclopedia

Paleobiota of the Posidonia Shale
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The Sachrang Formation or "Posidonienschiefer" Formation (common name the "Posidonia Shale") is a geological formation of southwestern Germany, northern Switzerland, northwestern Austria, southeast Luxembourg and the Netherlands, that spans about 3 million years during the Early Jurassic period (early Toarcian stage). It is known for its detailed fossils, especially marine biota, listed below.[1] Composed mostly of black shale, the formation is a Lagerstätte, where fossils show exceptional preservation (including exquisite soft tissues), with a thickness that varies from about 1 m to about 40 m on the Rhine level, being on the main quarry at Holzmaden between 5 and 14 m.[1] Some of the preserved material has been transformed into the fossil hydrocarbon jet which, especially jet derived from wood remains, is used for jewelry.[2] The exceptional preservation seen in the Posidonia Shale has been studied since the late 1800s, finding that a cocktail of chemical and environmental factors led to such an impressive preservation of the marine fauna.[2] The most common theory is that changes in the oxygen level, where the different anoxic events of the Toarcian left oxygen-depleted bottom waters, stopped scavengers from consuming the dead bodies.[3]

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18x6 m fossilized floating wood (Agathoxylon), with Crinoids attached (Pentacrinites & Seirocrinus). It is one of the most emblematic fossils of the formation, where the anoxic seas of the lower toarcian lead to an exquisite preservation.
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Biological interactions

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Seirocrinus subsingularis stems over a branch
  • The "Monotis"-Dactylioceras bed shows an accumulation of the bivalves Meleagrinella substriata and the ammonite Dactylioceras, that were the most abundant representatives of its group on the Altdorf region, and were probably washed to near epicontinental waters by a rapid event, or as result of a large succession of events.[4] This assemblage has been compared with modern Brazilian coastal mangroves and also linked to tsunami events.[5]
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Hybodus hauffianus with skin and Belemnnite traces
  • Several empty ammonite shells from Holzmaden have been found with associated decapods inside.[6] This includes a possible member of the genus Paleastacus inside a chamber of a Harpoceras.[6] This decapod is related to the family Erymidae, which are considered to be possible bottom-dweller carnivores or carrion feeders.[6] The associated fossil has several spherical structures that had been interpreted as decapod coprolites, implying that the animal lived for a long period within the shell.[6] More recent studies had recovered new data about the inquilinism of decapods inside ammonites, this time, however, recovering three eryonoids together within a body chamber.[7] The eryonoids most likely used the ammonoid as some kind of shelter, possibly due to the shell being an ideal location to molt, protection against predators, a source of food or that the shell was used as a long-term shelter.[7] One key aspect found was that the muddy bottom was not suitable for burrowing, implying that the decapods inhabited a different shelter due to being unable to make their own.[7] Other biota are found related to the decayed ammonite shells, such as serpulid annelids and bivalves, creating what was denominated as "benthic islands".[6]
  • Beyond trace fossils, several vertebrate specimens show associations with crustacean exoskeletal remains such as GPIT-PV-31586 and SMNS 58389 (Pachycormus macropterus) with necrophagous interaction as well SMNS 55934 (Stenopterygius quadriscissus) or SMNS 95401 (Metopacanthus sp.).[8]
  • The genus Clarkeiteuthis and its predatory behaviour, found associated with fishes of the genus Leptolepis.[9] Based on the position of prey and predator, it was suggested that the cephalopods caught and killed the fishes while the schools were still in well-oxygenated waters and then descended into oxygen-depleted water layers where the cephalopod suffocated and died attached to its prey.[9] The cephalopods’ arms were contracted over the fish, likely killing it quickly by cutting its spine.[9]
  • Several Geotheutis have been reported with eumelanin preserved along with their ink sacs.[10]
  • A specimen of Jeletzkyteuthis found in Ohmden has appeared predating a Parabelopeltis. The association of these 2 genera shows the predatory behaviour of this group when its members lived in epicontinental seas, which is rather different than extant Vampyromorphs.[11]
  • A pabulite (fossilized meal which never entered the digestive tract) was recovered from Holzmaden, being composed of an associated Passaloteuthis laevigata with its arms embracing an exuvia of a crustacean.[12] The belemnnite itself can be seen as the remnant of a failed predation attempt from a Hybodus, corroborating a possible tropic chain.[12]
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Stenopterygius quadriscissus, mother with embryo
  • One of the most complex organism interactions on the Posidonia Shale were the crinoid megarafts that grouped a wide variety of animals, creating large floating ecosystems.[13] The largest megaraft found measured 18 metres (59 ft), and is based on an Agathoxylon trunk, where different animals were attached.[13] The first attached animals would have been the growing community of oysters, bivalves and crinoids, that would add a small weight to the raft (about 800 kilograms (1,800 lb)).[13] The presence of these megarafts were in part possible due to the absence of marine wood worms which destroy tree logs in less than 3 years along with the absence of modern raft wood predators (that appeared on the Bathonian). These rafts could last up to 5 years, which is the main reason the crinoids attached were able to reach huge sizes.[13] These rafts were likely also essential to distribute animals along sea basins.[13] Seirocrinus & Pentacrinites were some of the main crinoid colonizers of the floating rafts.[14] Seirocrinus is the main representative of the pelagic crinoids, being among the longest animals known, reaching 26 m long in the largest documented specimen.[14] The ecology of the genus is widely known, with it being known that the smallest stems were among the first animals to colonize the rafts, with at least 2 generations of crinoids found per raft, where the hydrodynamic changes of the log influenced the settlement of the crinoids.[14] It is believed that Seirocrinus underwent seasonal reproduction linked to monsoonal conditions that sent new logs to the sea.[14] The large crinoids would have feed on pelagic micronutrients, and after the log fell to the bottom, all of the colony would have died.[14]
  • Thoracic barnacles of the genus Toarcolepas became the oldest epiplanktonic barnacle known in the fossil record, probably motivated by the appearance of the giant crinoid rafts. It has been found in situ associated with fossil wood.[15]
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Fossil of Clarkeiteuthis preying on Leptolepis
  • The shark Hybodus includes specimens with gastric contents full of belemnnite fragments.[16] This implies active predatory behaviour by the genus towards several kinds of belemnnites, such as Youngibelus.[16]
  • A speiballen (a regurgitated mass composed of indigestible stomach contents) had been found in the Holzmaden quarry.[17] The speiballen measures 285 mm in length with a diameter of 160 mm, and consists of 4 members of the genus Dapedium (Dapediidae) and a jaw identified as Lepidotes (Semionotidae).[17] The maker of this speiballen has been suggested to be a shark like Hybodus, an actinopterygian or a marine reptile.[17]
  • A specimen of Pachycormus has been found with stomach contents that include hooks similar to the ones found on genera like Clarkeiteuthis.[18]
  • Another specimen of Pachycormus macropterus preserves an ammonite inside its gut, likely swallowed by accident and directly responsible for the fish’s death.[19]
  • SMNS 51144 (Saurostomus esocinus) was found with Chondrites sp. burrows in the abdominal cavity, what indicates a possible opportunistic scavenger. Other Chondrites sp. includes SMNS 17500 and MHH 1981/25 (Stenopterygius uniter) that either suggest the ichthyosaurs were preserved immediately below one such bioturbation horizon or scavenger association.[8]
  • The known specimens of Toarcocephalus are evidence of successful predation events, as the head of one was isolated, likely as product of a decapitation, with another preserved within a regurgitated mass.[20]
  • One of the most emblematic finds of the formation is that of a mother Stenopterygius giving birth to live young. While specimens have been found with embryos, the bones of these embryos are scattered partly beyond the body limits of the mother.[21] There have been various theories about this scenario: either the bones of embryos had been deposited before the body of the adult went to the sea floor, or in the ichthyosaurs’ last moments where it sank to the bottom and may have given untimely birth to some of the foetuses, and finally another option follows post mortem hydrostatic pressure being too high to be prevented by the body, exploding or expelling its embryos.[22]
  • The specimen SMNS 53363 (Eurhinosaurus?) from Aichelberg was found with two encrusted large oysters (Liostrea) on the right pterygoid, considered to be part of a reef stage over bones.[8]
  • SMNS 80234 (Stenopterygius quadriscissus) represents another female with embryos, yet also shows ribs broken perimortem that may represent either intraspecific aggression or a predation attempt. This specimen has several taxa associated: ammonite aptychi, two ophiuroids (Sinosura brodiei) and a articulated echinoid (Diademopsis crinifera) indicate a short-lived deadfall community.[8]
  • SMNS 81841 (Stenopterygius quadriscissus) represents one of the clearest examples of deadfall communities described in the formation: the skeleton is associated with serpulids surrounded by a mass of disarticulated ophiuroid remains, indeterminate echinoid tests, an isolated crinoid ossicle, the byssate bivalve Oxytoma inaequivalvis, the pectinid Propeamussium pumilus, Eopecten strionatis, Plagiostoma sp., Meleagrinella sp., "Cucullaea" muensteri, with the genera Parainoceramya dubia and Liostrea associated with the carcass.[23] As many of these bivalves show overgrowth the community likely persisted for some time.[23] Fossil traces of Gastrochaenolites isp. attributed to mechanical bivalve borers are abundant implicating prolonged exposure of the skeleton on the seafloor.[23]
  • SMNS 81719 (Stenopterygius uniter) includes Liostrea, Propeamussium pumilus, Plagiostoma sp. and Parainoceramya dubia, with other invertebrates found (?) not being part of the deadfall community, such as several ammonites and Parainoceramya valves, being stratigraphically below the specimen.[8] This specimen includes also traces of scavenging activity, possibly by crustaceans.[8]
  • SMNS 80113, (Stenopterygius triscissus) was found populated by Parainoceramya, a specimen of Eopecten strionatis and an unexpected specimen of the small infaunal lucinid Mesomiltha pumila, equivocal evidence for the sulfophilic stage.[8]
  • Local ichthyosaur soft tissues include skin enough well preserved to infer coloration and appearance on the living animal, as well evidence for homeothermy and crypsis.[24]
  • Gut contents of the local pterosaurs are known: Campylognathoides preserves hooks of the coleoid Clarkeiteuthis (therefore being the one of the few teuthophagous pterosaurs), while Dorygnathus preserves remains of Leptolepis.[25]
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Microbial activity

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Non-fenestrate stromatolite crusts formed in aphotic deep-water environments during intervals of very low sedimentation are recovered in places such as Teufelsgraben, Hetzles.[26] The stromatolites of this region have evidence of live on a deeper shelf environment with a quietwater deposit which suffered repeated phases of stagnant bottom waters, where a depth water habitat developed, probably at more than 100 meters depth.[26] There is a thin, southern widespread stromatolite crust on the top of the Sachrang Formation, called "Wittelshofener Bank", that has made researchers rethink the depth of the major southern basin of the formation, where the absence of phototrophic calcareous benthic organisms (probably due to the lack of light) shows the depth of the basin.[26] On the "Wittelshofener Bank" there is also the only occurrence of ooids, presumably formed in the same deep-water environment.[26]

Color key
Taxon Reclassified taxon Taxon falsely reported as present Dubious taxon or junior synonym Ichnotaxon Ootaxon Morphotaxon
Notes
Uncertain or tentative taxa are in small text; crossed out taxa are discredited.
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Cyanobacteria

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Rhizaria

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Foraminifera

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Dinoflagellata

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Dinoflagellate cysts

The evolutionary burst of the Toarcian dinoflagellates led the first appearance and rapid radiation of the Phallocystaceae (Susainium, Parvocysta, Phallocysta, Moesiodinium and related forms).[30] This occurred at the time of a widespread Lower Toarcian bituminous anoxia-derived shale, which is recovered from the Posidonienschiefer, Pozzale, Italy, Asturias, Spain, Bornholm, Denmark, the Lusitanian Basin of Portugal, the Jet Rock Formation in Yorkshire and to the "Schistes Carton" in northern France. Whether there is a causal connection in this co-occurrence of Phallocystaceae and bituminous facies is a problem still to be resolved. This family has its acme in diversity and quantity in the latest Toarcian and became less important in the Aalenian.[30]

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Algae

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The Posidonia Shale preserves an abundant variety of algae, such as the genus of colonial green algae Botryococcus, or the unicellular algal bodies Tasmanites, and other small examples. Algae are a good reference for changes on the oxygen conditions along the Toarcian.[37]

Algal acritarchs

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Haptophyta

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Chlorophyta

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Fungi

Fungal spores, hyphae and indeterminate remains are a rare element of the otherwise open marine deposits of the Posidonienschiefer formation, but were recovered at Dormettingen.[46] These fungal remains are composed mostly of indeterminate spores and indicate oxygenated environments and suitable transportation by rivers.[46]

Incertae sedis

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Ichnofossils

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The major ichnological analyses of the Posidonian Shale come from Dotternhausen/Dormettingen, where the ichnogenus Phymatoderma formed the so-called Tafelfleins and Seegrasschiefer.[48] The Tafelflein bed was deposited under anoxic bottom and pore water, where a recover of oxygen allow the Phymatoderma-producers return.[48] The two organic-rich layers (Tafelfleins and Seegrasschiefer) are characterized by the dense occurrence of trace fossils such as Chondrites and Phymatoderma, done episodically due to the fall of the oxygen levels.[48] The coeval more nearshore Swiss deposits referred Posidonian Shale (Rietheim Member) hosted similar trace fossils to those recovered on SW Germany.[48] Ichnofossils in this setting apparently evolved faster to more oxic-to-dysoxic bottom waters.[48] At Unken, laminated deposits of red limestone suggest well oxygenated active waters (as they lack shale), where high amounts of Chondrites are found.[40]


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Invertebrata

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Porifera

In the non-bituminous facies located on Obereggenen im Breisgau (Shore of the Black Forest High), especially the lower semicelatum subzone, pyritized individual needles of silica sponges (Demospongiae and Hexactinellida) are found, rarely on pelagic layers to very often on the low depth marine deposits.[27] They are usually associated with radiolarian stone cores. In Dusslingen and Reutlingen, these sponge needles are sometimes barytized in phosphorites of the Haskerense subzone and are much more common here than in any other zone of the Lower Toarcian. These needles are absent in the bituminous horizons of the entire Lower Toarcian.[27] Increased amounts of sponge needles (dominated by Hexactinellida) are also found on the arenaceous facies of the nearshore unit that is the Unken member, being the only section if its region hosts them, probably due to be an active and well oxygenated bottom.[40] The location of this member as a possible bay on the south of the vindelician land probably allow to the development of more pre-Toarcian AOE conditions, hence the presence of biota otherwise rare on bituminous layers.[40]

Annelida

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Lophophorata

Bryozoa

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Brachiopoda

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Mollusca

Bivalvia

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Gastropoda

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Cephalopoda

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Crustacea

Cycloidea

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Ostracoda

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Malacostraca

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Thoracica

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Arachnida

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Insecta

Incertae sedis

Insects are common terrestrial animals that were probably washed into the sea due to monsoon conditions present on the Sachrang Formation.[126]

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Notoptera

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Eoblattida

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Odonatoptera

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Odonata

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Orthoptera

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Dictyoptera

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Hemiptera

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Hymenoptera

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Neuroptera

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Hemiptera

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Coleoptera

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Amphiesmenoptera

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Miscellaneous (incl. Diptera)

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Echinodermata

Echinoderm debris is relatively abundant in the shale-free Unken and Salzburg members, including crinoid and brittle star skeletal elements; sea urchins take their place later in the formation, with them having especially diversified at that time, leading to pedicellaria being observed very often.[40]

Asterozoa

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Echinoidea

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Holothuroidea

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Crinoidea

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Vertebrata

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Fishes

Chondrichthyes

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Actinopterygii

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Sarcopterygii

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Amniota

Ichthyosauria

Inderminate specimens are known.[29][195][196][197]

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Plesiosauria

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Sphenodontia

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Testudinata

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Crocodylomorpha

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Pterosauria

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Dinosauria

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Plantae

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The Flora is dominated by horsetails, which may be in a similar ecological niche to the modern genus Phragmites, able to resist saline conditions. Storms or floods may be the major events that transported this flora to the sea.

The macroflora of the Posidonia Slate can be described as extremely poor in species.[262] Apart from the remains of horsetails, it is without exception the remains of coarse branches and fronds from gymnosperms, which can be assumed were transport resistant. Remains of ferns are completely missing, except for tall arboreal ferns (Peltaspermales).[263] Most of the flora was reported from the area of Braunschweig.[262] The major explanation for this flora could be that the plants in question are mono-or oligotypic stands on the edge of the waters that flowed into the Posidonienschiefer sea, probably torn away in flood events, easily fragmented during transport and from waves, especially in the occasional storm events postulated.[264] In terms of taphonomy, this would result in a comparison with today's reed Phragmites, which can form extensive stocks on the edge of shallow and slowly flowing waters.[262] The wood remnants clearly indicate higher diversity of coniferous flora in the delivery area than remains of leafy branches.[262] This fact is likely to be proportionate, similar to the frequent occurrence of charcoalized trunks, most of them are believed to be "driftwoods" which spent a long time drifting, and this also suggests frequent settlement with mussels and full-grown crinoids.[262][264] The deposition settings are a large distance from the nearest coastline (for southern Germany about 100 kilometers), making only plants resistant to transportation able to survive long enough to get deposited.[265][141] At Irlbach and Kheleim, NE of Regensburg, where the Posidonienschiefer has a near mainland deposit with abundant sand, a rich deposit filled with plant remains of different kinds (Seeds, reproductive organs, leaves, stems, cuticles and wood) with traces of coal was recovered, however, it was never studied in depth.[78] Of all the plant material excavated only a few bennettite leaves and two conifer branches with leaves were cited and none studied.[78] In the Austrian sites the Sachrang Member was developed in the basinal area, while the Unken Member, sandwiched between red, often condensed limestones, represents the marginal facies.[40] Due to being more marginal and connected with the southern Vindelician land, the most diverse palynological assemblages of the formation are found transported from zones with moldanuvian granites as proven by the feldspar accumulations.[40]

Phytoclasts

Phytoclasts have been recovered from several sections on the formation, but only studied in depth from the Dotternhausen and specially Dormettingen.[46] Here two kinds of phytoclasts were recovered, opaque phytoclasts (charcoal, indicator of wildfire activity on nearby landmasses, indicator of seasonal alterations of the water column) and translucent phytoclasts (indicator of proximal landmasses with high availability of wood and other plant material, as well as transport conditions).[46] On the lowermost part of the section opaque phytoclasts are low (15% of the total organic matter) while translucent are incredibly abundant (40%), lowering to around 20-10% on the next section.[46] The Exaratum subzone is the only one with an inverse trend and more abundance of opaque phytoclasts. On the Bifrons level, both types reach between a 15% and a 30%, showing a rapid increase, then decreasing at the end of the section to values of less than 10%.[46] Opaque Phytoclasts, for a supposed marine deposit are relatively abundant on some sections, while their decreasing levels suggest (along with increasing levels of Kaolinite) an increased delivery of land plant material by rivers, from areas with wetter climate and less frequent fires, while its rise suggests the opposite, a nearby continental setting with dry climate and continuous wildfire activity.[46]

Palynology

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Equisetaceae

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Pteridospermatophyta

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Bennettitales

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Ginkgoales

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Pinophyta

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Fossil wood

Fossil wood amount increases in the marginal Unken Member, with great amounts of logs and fragments more than 1 m long. Surface studies suggest relationships with the wood genera identified on the coeval Úrkút Manganese Ore Formation.[282]

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References

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