Early Oligocene to Pliocene Colubridae of Europe: a review

2012 ◽  
Vol 183 (6) ◽  
pp. 661-681 ◽  
Author(s):  
Zbigniew Szyndlar
Keyword(s):  
Early Miocene ◽  
Dominant Group ◽  
European Continent ◽  
Fossil Species ◽  
Early Pliocene ◽  
Early Oligocene ◽  
Living Species ◽  
The Rich ◽  
Europe Today ◽  
Almost All

Abstract The paper reviews the entire fossil record of the Colubridae coming from the European Early Oligocene (MP21) to late Early Pliocene (MN15) localities. Prior to the end of the Early Miocene, European colubrids were rare and dominated by booid snakes. At the end of the Early Miocene (MN4), the archaic ophidian fauna of Europe was literally flooded by eastern immigrants, principally representatives of the colubroid families Colubridae, Elapidae, and Viperidae. Since then, the Colubridae became a dominant group in snake assemblages, both in Europe and elsewhere. The rich colubrid fauna inhabiting the European continent in the Middle Miocene (MN5 to 7+8) was composed exclusively of extinct species, representing mainly fossil genera, although members of living genera were also quite common. At the beginning of the Late Miocene (MN9), almost all fossil genera became extinct, but living genera were represented exclusively by fossil species. In the late Early Pliocene (MN15), almost all European colubrids were living species. The Late Pliocene (MN16) and Pleistocene colubrid snakes did not differ from those inhabiting Europe today.

scholarly journals The early Miocene flora of Güvem (Central Anatolia, Turkey): a window into early Neogene vegetation and environments in the Eastern Mediterranean

2017 ◽  
Vol 57 (2) ◽  
pp. 237-338 ◽  
Author(s):  
Thomas Denk ◽  
Tuncay H. Güner ◽  
Zlatko Kvaček ◽  
Johannes M. Bouchal
Keyword(s):  
Eastern Mediterranean ◽  
Central China ◽  
Early Miocene ◽  
Central Anatolia ◽  
Substantial Part ◽  
Swamp Forest ◽  
Fossil Species ◽  
Biogeographic Patterns ◽  
Plant Assemblage ◽  
The Rich

AbstractThe early Burdigalian (MN3) plant assemblage of the Güvem area (northwestern Central Anatolia) is preserved in lacustrine sediments of the Dereköy pyroclastics. Its age is well constrained by radiometric dates of basaltic rocks bracketing the pyroclastics, making the Güvem flora one of the extremely few precisely dated early Miocene floras in the Mediterranean region. The rich assemblage of impression fossils comprises ferns and fern allies (2 species), gymnosperms (12 spp.) and angiosperms (129 spp.).Ilex miodipyrenasp. nov. is described as a new fossil-species. The most diverse families in the assemblage are the Fagaceae with 12 taxa and the Fabaceae with 12 leaf morphotypes and one fruit taxon. Aquatic plants are represented by seven taxa, riparian (including palms) and swamp forest elements by >35 taxa, and lianas by three taxa (Smilaxspp.,Chaneya). The relatively large number of aquatic and riparian/swamp elements is congruent with the rich fish, amphibian and reptile record of the Güvem area. Another characteristic feature of the plant assemblage is the presence of various lobed leaves which show similarities with modern species of different families (e.g.Alangium, various Malvales). Trees and shrubs growing on well-drained soils and forming closed-canopy and open-canopy forests are the most diversified group (>70 taxa). In terms of number of specimens in the collection and based on field observations, by far the most abundant leaf fossils belong to evergreen oaks ofQuercus drymejaandQ. mediterraneaand to various types of foliage that cannot be assigned to a particular extant or extinct genus of Fagaceae. These sclerophyllous trees must have covered vast areas surrounding the wetlands that developed during the early Miocene in the Güvem Basin. Based on a recent reassessment of the ecology and taxonomic affinity of these trees, they are considered to reflect humid temperate climatic conditions but with a brief drier season during the winter months. These forests are more similar to the laurel forests of the southeastern United States and those stretching in a narrow belt south of the Himalayas to eastern central China. The large number of Fabaceae may indicate the presence of warm subtropical environments but this is difficult to assess, as they are known for having wide ecological ranges today and in the past. All in all, a larger part of the plant taxa point to forested vegetation. This is in agreement with previous palynological studies which detected only small amounts of herbaceous and grass pollen. Open patches of vegetation may have been restricted to river banks and to rocky areas in a volcanic landscape. The biogeographic patterns detected for the early Miocene of the Güvem assemblage are manifold; most taxa are widespread Northern Hemispheric elements. A substantial part of the species migrated from Asia into Europe during the (late) Paleogene and reached Anatolia during the early Miocene (Fagus,Paliurus,Chaneya,Ailanthus,Quercus kubinyii,Davallia haidingeri,Acer angustilobum,A. palaeosaccharinum). Fewer taxa may have been in Anatolia before they migrated to Europe (e.g.Nerium,Smilax miohavanensis,Quercus sosnowskyi). Finally, very few taxa are Anatolian endemics (e.g.Ilex miodipyrena).

Stratigraphic Intervals for Oil and Tar Sand Deposits in the Uinta Basin, Utah

2017 ◽  
Vol 54 (4) ◽  
pp. 227-264
Author(s):  
Ronald Johnson ◽  
Justin Birdwell ◽  
Paul Lillis
Keyword(s):  
Brackish Water ◽  
Source Rocks ◽  
Uinta Basin ◽  
Green River ◽  
Reservoir Rocks ◽  
Stratigraphic Framework ◽  
Two Samples ◽  
The Rich ◽  
And Migration ◽  
Almost All

To better understand oil and bitumen generation and migration in the Paleogene lacustrine source rocks of the Uinta Basin, Utah, analyses of 182 oil samples and tar-impregnated intervals from 82 core holes were incorporated into a well-established stratigraphic framework for the basin. The oil samples are from the U.S. Geological Survey Energy Resources Program Geochemistry Laboratory Database; the tar-impregnated intervals are from core holes drilled at the Sunnyside and P.R. Spring-Hill Creek tar sands deposits. The stratigraphic framework includes transgressive and regressive phases of the early freshwater to near freshwater lacustrine interval of Lake Uinta and the rich and lean zone architecture developed for the later brackish-to-hypersaline stages of the lake. Two types of lacustrine-sourced oil are currently recognized in the Uinta Basin: (1) Green River A oils, with high wax and low β-carotane contents thought to be generated by source rocks in the fresh-to-brackish water lacustrine interval, and (2) much less common Green River B oils, an immature asphaltic oil with high β-carotane content thought to be generated by marginally mature to mature source rocks in the hypersaline lacustrine interval. Almost all oil samples from reservoir rocks in the fresh-to-brackish water interval are Green River A oils; however four samples of Green River A oils were present in the hypersaline interval, which likely indicates vertical migration. In addition, two samples of Green River B oil are from intervals that were assumed to contain only Green River A oil. Tar sand at the P.R. Spring-Hill Creek deposit are restricted to marginal lacustrine and fluvial sandstones deposited during the hypersaline phase of Lake Uinta, suggesting a genetic relationship to Green River B oils. Tar sand at the Sunnyside deposit, in contrast, occur in marginal lacustrine and alluvial sandstones deposited from the early fresh to nearly freshwater phase of Lake Uinta through the hypersaline phase. The Sunnyside deposit occurs in an area with structural dips that range from 7 to 14 degrees, and it is possible that some tar migrated stratigraphically down section.

scholarly journals The Cenozoic Malaguide Basin from Sierra Espuña (Murcia, S Spain): An Example of Geological Heritage

Geosciences ◽  
2021 ◽  
Vol 11 (1) ◽  
pp. 34
Author(s):  
Santiago Moliner-Aznar ◽  
Manuel Martín-Martín ◽  
Tomás Rodríguez-Estrella ◽  
Gregorio Romero-Sánchez
Keyword(s):  
Middle Eocene ◽  
Geological Heritage ◽  
Passive Margin ◽  
Early Miocene ◽  
Late Oligocene ◽  
Deep Basin ◽  
Sedimentary Evolution ◽  
Early Oligocene ◽  
Upper Oligocene ◽  
Very High

The Cenozoic Malaguide Basin from Sierra Espuña (Internal Betic Zone, S Spain) due to the quality of outcropping, areal representation, and continuity in the sedimentation can be considered a key-basin. In the last 30 years, a large number of studies with very different methodological approaches have been done in the area. Models indicate an evolution from passive margin to wedge-top basin from Late Cretaceous to Early Miocene. Sedimentation changes from limestone platforms with scarce terrigenous inputs, during the Paleocene to Early Oligocene, to the deep basin with huge supplies of turbidite sandstones and conglomerates during the Late Oligocene to Early Miocene. The area now appears structured as an antiformal stack with evidence of synsedimentary tectonics. The Cenozoic tectono-sedimentary basin evolution is related to three phases: (1) flexural tectonics during most of the Paleogene times to create the basin; (2) fault and fold compartmentation of the basin with the creation of structural highs and subsiding areas related to blind-fault-propagation folds, deforming the basin from south to north during Late Oligocene to Early Aquitanian times; (3) thin-skin thrusting tectonics when the basin began to be eroded during the Late Aquitanian-Burdigalian. In recent times some works on the geological heritage of the area have been performed trying to diffuse different geological aspects of the sector to the general public. A review of the studies performed and the revisiting of the area allow proposing different key-outcrops to follow the tectono-sedimentary evolution of the Cenozoic basin from this area. Eight sites of geological interest have been selected (Cretaceous-Cenozoic boundary, Paleocene Mula Fm, Lower Eocene Espuña-Valdelaparra Fms, Middle Eocene Malvariche-Cánovas Fms, Lowermost Oligocene As Fm, Upper Oligocene-Lower Aquitanian Bosque Fm, Upper Oligocene-Aquitanian Río Pliego Fm, Burdigalian El Niño Fm) and an evaluation has been performed to obtain four parameters: the scientific value, the educational and touristic potential, and the degradation risk. The firsts three parameters obtained values above 50 being considered of “high” or “very high” interest (“very high” in most of the cases). The last parameter shows always values below 50 indicating a “moderate” or “low” risk of degradation. The obtained values allow us considering the tectono-sedimentary evolution of this basin worthy of being proposed as a geological heritage.

scholarly journals Late oligocene–early miocene shortening in the Thrace Basin, northern Aegean

2021 ◽  
Author(s):  
Ümitcan Erbil ◽  
Aral I. Okay ◽  
Aynur Hakyemez
Keyword(s):  
Large Scale ◽  
Middle Eocene ◽  
Early Miocene ◽  
Fold Axis ◽  
Late Oligocene ◽  
The Balkans ◽  
Sedimentary Sequences ◽  
The North ◽  
Early Oligocene ◽  
Thrace Basin

AbstractLate Cenozoic was a period of large-scale extension in the Aegean. The extension is mainly recorded in the metamorphic core complexes with little data from the sedimentary sequences. The exception is the Thrace Basin in the northern Aegean, which has a continuous record of Middle Eocene to Oligocene marine sedimentation. In the Thrace Basin, the Late Oligocene–Early Miocene was characterized by north-northwest (N25°W) shortening leading to the termination of sedimentation and formation of large-scale folds. We studied the stratigraphy and structure of one of these folds, the Korudağ anticline. The Korudağ anticline has formed in the uppermost Eocene–Lower Oligocene siliciclastic turbidites with Early Oligocene (31.6 Ma zircon U–Pb age) acidic tuff beds. The turbidites are underlain by a thin sequence of Upper Eocene pelagic limestone. The Korudağ anticline is an east-northeast (N65°E) trending fault-propagation fold, 9 km wide and 22 km long and with a subhorizontal fold axis. It is asymmetric with shallowly-dipping northern and steeply-dipping southern limbs. Its geometry indicates about 1 km of shortening in a N25°W direction. The folded strata are unconformably overlain by Middle Miocene continental sandstones, which constrain the age of folding. The Korudağ anticline and other large folds in the Thrace Basin predate the inception of the North Anatolian Fault (NAF) by at least 12 myr. The Late Oligocene–Early Miocene (28–17 Ma) shortening in the Thrace Basin and elsewhere in the Balkans forms an interlude between two extensional periods, and is probably linked to changes in the subduction dynamics along the Hellenic trench.

Three new cribrimorph bryozoans (order Cheilostomatida) from the early Miocene of Argentina, with a discussion on spinocystal shield morphologies

2021 ◽  
pp. 1-15
Author(s):  
Juan López-Gappa ◽  
Leandro M. Pérez ◽  
Ana C.S. Almeida ◽  
Débora Iturra ◽  
Dennis P. Gordon ◽  
...  
Keyword(s):  
Type Species ◽  
Systematic Position ◽  
Early Miocene ◽  
Morphological Data ◽  
Fossil Species ◽  
Extant Species ◽  
The Family ◽  
Subjective Synonym

Abstract Bryozoans with calcified frontal shields formed by the fusion of costae, collectively constituting a spinocyst, are traditionally assigned to the family Cribrilinidae. Today, this family is regarded as nonmonophyletic. In the Argentine Cenozoic, cribrilinids were until recently represented by only two fossil species from the Paleocene of Patagonia. This study describes the first fossil representatives of Jolietina and Parafigularia: J. victoria n. sp. and P. pigafettai n. sp., respectively. A fossil species of Figularia, F. elcanoi n. sp., is also described. The material comes from the early Miocene of the Monte León and Chenque formations (Patagonia, Argentina). For comparison, we also provide redescriptions of the remaining extant species of Jolietina: J. latimarginata (Busk, 1884) and J. pulchra Canu and Bassler, 1928a. The systematic position of some species previously assigned to Figularia is here discussed. Costafigularia n. gen. is erected, with Figularia pulcherrima Tilbrook, Hayward, and Gordon, 2001 as type species. Two species previously assigned to Figularia are here transferred to Costafigularia, resulting in C. jucunda n. comb. and C. tahitiensis n. comb. One species of Figularia is reassigned to Vitrimurella, resulting in V. ampla n. comb. The family Vitrimurellidae is here reassigned to the superfamily Cribrilinoidea. The subgenus Juxtacribrilina is elevated to genus rank. Inferusia is regarded as a subjective synonym of Parafigularia. Parafigularia darwini Moyano, 2011 is synonymized with I. taylori Kuklinski and Barnes, 2009, resulting in Parafigularia taylori n. comb. Morphological data suggest that these genera comprise different lineages, and a discussion on the disparities among cribrilinid (sensu lato) spinocysts is provided. UUID: http://zoobank.org/215957d3-064b-47e2-9090-d0309f6c9cd8

Ocotea dilcherii, a new name for Ocotea obtusifolia (Berry) LaMotte (Lauraceae)

Phytotaxa ◽  
2015 ◽  
Vol 239 (2) ◽  
pp. 199
Author(s):  
Sergei Vasilyevich Vikulin
Keyword(s):  
Natural History ◽  
Type Specimen ◽  
Valid Species ◽  
Early Eocene ◽  
National Museum ◽  
Mississippi Embayment ◽  
Fossil Species ◽  
Early Oligocene ◽  
Leaf Remains ◽  
Nomen Novum

The fossil species  Oreodaphne obtusifolia Berry (1916: 301) was described, based on the fossil leaf remains of the most abundant laurel from the Early Eocene Wilcox Group sediments of Holly Springs: Marshall Co, Grenada Co., Miss.: Mississippi embayment (Southeastern North America). Nowadays, most systematists consider the extant Oreodaphne to be a member of Ocotea (Mez, 1889: 219; Rohwer, 1986; van der Werff, 2002; Chanderbali et al., 2001). LaMotte (1952) transferred Berry’s (1916: 301) combination to Ocotea, and this transfer was followed by Dilcher (1963), who reinforced attribution of Wilcox leaf megafossils to Ocotea by cuticular analysis of epidermis and stomata (Dilcher & Lott, 2005). However, according to Art. 53.1 of the ICN (McNeill et al.  2012) the name Ocotea obtusifolia (Berry) LaMotte (1952) is illegitimate because of the existence of the earlier overlooked homonym, Ocotea obtusifolia Kunth (1817: 165–166), an extant lauraceous species from Colombia (Muséum National d’Histoire Naturelle, holotype: http://plants.jstor.org/stable/10.5555/al.ap.specimen.P00128771). The homonymy between these fossil and extant American species of Ocotea was revealed during the description of the new fossil Early Oligocene species Ocotea rossica Vikulin from the south of the Middle-Russian upland (Vikulin, 2015: 326). Since Ocotea obtusifolia (Berry) LaMotte has been systematically recognized as a valid species in current use and it does not have any synonym, a nomen novum, O. dilcherii, is formally proposed here as a replaced name. Because a type specimen was not indicated among the validating illustrations of Berry (1916: pl. 80, fig. 1; pl. 83, fig. 2–5, and pl. 84, fig. 1 and 2), a lectotype must be designated here, from the specimens illustrated in the protologue (Berry, 1916: 301–302) amongst those perfect specimens with blunt leaf apex, which are very abundant in the clays at Puryear, Tenn. (Proposed lectotype: paleobotany collection # USNM 35867, Smithsonian National Museum of Natural History (USA), illustrated in Berry, 1916: 301, pl. 83, fig. 5.

scholarly journals New phiocricetomyine rodents (Hystricognathi) from the Jebel Qatrani Formation, Fayum Depression, Egypt

PeerJ ◽  
2021 ◽  
Vol 9 ◽  
pp. e12074
Author(s):  
Shorouq F. Al-Ashqar ◽  
Erik R. Seiffert ◽  
Dorien de Vries ◽  
Sanaa El-Sayed ◽  
Mohamed S. Antar ◽  
...  
Keyword(s):  
New World ◽  
New Genus ◽  
Late Eocene ◽  
Type Locality ◽  
New Genus And Species ◽  
Additional Material ◽  
Early Oligocene ◽  
Species Type ◽  
The Rich ◽  
Latest Eocene

Background The rich rodent assemblages from the Eocene–Oligocene deposits of the Jebel Qatrani Formation (Fayum Depression, Egypt) have important implications for our understanding of the origin and paleobiogeography of Hystricognathi, a diverse clade that is now represented by the Afro-Asiatic Hystricidae, New World Caviomorpha, and African Phiomorpha. Methods Here we present previously undescribed material of the enigmatic hystricognath clade Phiocricetomyinae, from two stratigraphic levels in the lower sequence of the Jebel Qatrani Formation—a new genus and species (Qatranimys safroutus) from the latest Eocene Locality 41 (~34 Ma, the oldest and most productive quarry in the formation) and additional material of Talahphiomys lavocati from that species’ type locality, early Oligocene Quarry E (~31–33.2 Ma). Results The multiple specimens of Qatranimys safroutus from L-41 document almost the entire lower and upper dentition, as well as mandibular fragments and the first cranial remains known for a derived phiocricetomyine. Specimens from Quarry E allow us to expand comparisons with specimens from Libya (late Eocene of Dur at-Talah and early Oligocene of Zallah Oasis) that have been placed in T. lavocati, and we show that the Dur at-Talah and Zallah specimens do not pertain to this species. These observations leave the Fayum Quarry E as the only locality where T. lavocati occurs.

scholarly journals A New Cypselomorph Bird from the Middle Eocene of Germany and the Early Diversification of Avian Aerial Insectivores

The Condor ◽  
2005 ◽  
Vol 107 (2) ◽  
pp. 342-352 ◽  
Author(s):  
Gerald Mayr
Keyword(s):  
Phylogenetic Analysis ◽  
Middle Eocene ◽  
Sister Group ◽  
Food Competition ◽  
Early Miocene ◽  
New Taxon ◽  
Insectivorous Birds ◽  
Dominant Group ◽  
Early Diversification ◽  
Aerial Insectivores

Abstract A new taxon of the Cypselomorphae—the clade including nightjars, potoos, owlet-nightjars, and apodiform birds—is described from the middle Eocene of Messel in Germany. Phylogenetic analysis of 49 characters shows Protocypselomorphus manfredkelleri gen. et sp. nov. to be the sister group of all other cypselomorph taxa, although this placement was not robust to bootstrapping. As evidenced by its swift-like beak, long forearm, and reduced feet, P. manfredkelleri was hawking insects on the wing. Thus it adds a distinctive new taxon to the already diverse assemblage of Paleogene aerial insectivores, all of which belong to the Cypselomorphae. This strongly contrasts with the extant avifauna where many aerial insectivores belong to songbirds, and among the insectivorous cypselomorph taxa only swifts and nightjars are species rich and widely distributed. The diversity of aerial insectivores among the Cypselomorphae may have been reduced by food competition with songbirds, which do not become the dominant group of insectivorous birds before the early Miocene. Una Nueva Ave Cipselomorfa del Eoceno Medio de Alemania y la Diversificación Temprana de las Aves Insectívoras Aéreas Resumen. Se describe un nuevo taxón de Cypselomorphae, el clado que incluye a las familias Caprimulgidae, Nyctibiidae, Aegothelidae y a las aves apodiformes, del Eoceno medio de Messel en Alemania. Un análisis filogenético de 49 caracteres muestra que Protocypselomorphus manfredkelleri gen. et sp. nov. es el grupo hermano de los demás taxa de cipselomorfos, aunque esta posición no fue apoyada por el análisis de bootstrap. Como lo evidencia su pico tipo vencejo, antebrazo largo y patas pequeñas, P. manfredkelleri cazaba insectos al vuelo. Así, este hallazgo añade un nuevo taxón al grupo ya diverso de los insectívoros aéreos del Paleógeno, todos los cuales pertenecen al grupo de los cipselomorfos. Esto contrasta fuertemente con la avifauna actual, en que muchos insectívoros aéreos pertenecen al grupo de los paseriformes, mientras que de los taxa de insectívoros cipselomorfos sólo los apodiformes y caprimúlgidos presentan alta diversidad específica y se encuentran ampliamente distribuidos. La diversidad de los insectívoros aéreos en los cipselomorfos pude haberse reducido debido a la competencia por alimento con las aves paseriformes, las cuales no se transforman en el grupo dominante de aves insectívoras sino hasta el Mioceno temprano.

Early Miocene shallow-water corals from La Guajira, Colombia: Part II, Mussidae–Siderastreidae and Milleporidae

2018 ◽  
Vol 93 (3) ◽  
pp. 416-436 ◽  
Author(s):  
Paola Flórez ◽  
Paula Zapata-Ramírez ◽  
James S. Klaus
Keyword(s):  
Shallow Water ◽  
The Other ◽  
Early Miocene ◽  
Caribbean Region ◽  
Coral Fauna ◽  
Living Species ◽  
The Caribbean ◽  
Established Species ◽  
Zooxanthellate Corals

AbstractIn this contribution we describe and illustrate 14 coral morphospecies collected from the early Miocene Siamaná (Aquitanian–Burdigalian) and Jimol (late Burdigalian) formations of the Cocinetas Basin in La Guajira Peninsula, northern Colombia. Eleven were identified as already established species including seven genera belonging to the families Mussidae, Pocilloporidae, Poritidae, Siderastreidae, and Milleporidae; the other three remain in open nomenclature. Nine of the 11 species identified (81%) are extinct. The remaining two living species,Siderastrea sidereaandMillepora alcicornis, are common on modern Caribbean reefs. Their presence in the Siamaná Formation extends their temporal range in the Caribbean region to the early Miocene. Most of the taxa described here were hermatypic and zooxanthellate corals of the order Scleractinia, with the exception of the fire coralMillepora alcicornis, of the order Anthothecata, family Milleporidae. The coral fauna recorded in the Siamaná and Jimol formations is typical of shallow and calm waters of the Oligocene–Miocene transition.

Exploring the Ar isotope record of an early Miocene pseudotachylyte in an early Oligocene intrusion (Rieserferner pluton, eastern Alps)

Lithos ◽  
2019 ◽  
Vol 338-339 ◽  
pp. 1-17 ◽  
Author(s):  
Gianfranco Di Vincenzo ◽  
Giorgio Pennacchioni ◽  
Michel Bestmann
Keyword(s):  
Eastern Alps ◽  
Early Miocene ◽  
Early Oligocene ◽  
Isotope Record
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