An early heron (Aves, Ardeidae, Ardea) from the Middle Miocene of Nebraska

1986 ◽  
Vol 60 (4) ◽  
pp. 968-970 ◽  
Author(s):  
Jonathan J. Becker
Keyword(s):  
Brown Coal ◽  
Middle Miocene ◽  
Mining District ◽  
Large Species ◽  
Local Fauna ◽  
Fossil Species ◽  
Specific Identification ◽  
Upper Miocene ◽  
Living Species

The genus Ardea includes all living species of large herons. Brodkorb (1963) listed five fossil species of Ardea, and only one fossil species has since been described. Of these six, only two are unquestionably members of the genus Ardea. Ardea brunhuberi von Ammon, 1918, from the Upper Miocene Brown Coal Formation, Württemburg, Germany, was moved by Brodkorb (1980) to the Phalacrocoracidae as Phalacrocorax brunhuberi. Brodkorb (1980) considered A. lignitum Giebel, 1860, from the Sarmatian Brown Coal of Rippersroda, Thuringia, Germany, to be a large owl in the genus Bubo. Olson (1985) similarly regards A. perplexa from the Astaracian of Sansan, France, to be a large owl, possibly in the genus Bubo. The type of Ardea aureliensis Milne-Edwards, 1871, from the Oreleanian of Suevres, France, has never been illustrated or restudied and its affinities need to be confirmed (Olson, 1985). The valid fossil species are Ardea polkensis Brodkorb, 1955, from the late Hemphillian Bone Valley Mining District, Florida, and A. howardae Brodkorb, 1980, from the Plio/Pleistocene Shungura Formation, Omo Basin, Ethiopia. A large species of Ardea is also known from the late Clarendonian Love Bone Bed local fauna, Florida, but is based on material too fragmentary for specific identification (Becker, 1985). This note reports the earliest certain occurrence of Ardea now known.

Two new genera of peccaries (Mammalia, Artiodactyla, Tayassuidae) from upper Miocene deposits of the Amazon Basin

2012 ◽  
Vol 86 (5) ◽  
pp. 852-877 ◽  
Author(s):  
Carl David Frailey ◽  
Kenneth E. Campbell
Keyword(s):  
South America ◽  
Amazon Basin ◽  
Middle Miocene ◽  
South American ◽  
New Genera ◽  
Upper Miocene ◽  
General Similarity ◽  
Pecari Tajacu ◽  
Living Species ◽  
Ground Sloths

Two new, extinct taxa of peccaries from upper Miocene deposits of the western Amazon Basin provide the first data documenting the presence of these North American mammals in South America in the Miocene. One, Sylvochoerus woodburnei n. gen. n. sp., is allied morphologically to Tayassu pecari, whereas the second, Waldochoerus bassleri n. gen. n. sp., is more similar to Pecari tajacu. Both new taxa reflect an intermediate position between middle Miocene peccaries and modern Tayassu and Pecari. The specimens reported here were unstudied, but when collected they were referred to living species of Tayassu and Pecari based on their general similarity to species of those two living genera, and they were dated to the Pleistocene, presumably based on a long–standing model of the Great American Faunal Interchange. The presence of peccaries in South America at approximately the same time that South American ground sloths began appearing in upper Miocene deposits of North America, and soon after the appearance of gomphotheres in South America, indicates that dispersal between the Americas was earlier and involved more taxa than previously interpreted. Molecular divergence data are consistent, in part, with a late Miocene dispersal of peccaries to South America.

scholarly journals An integrated approach to the coal deposits in the Mesohellenic Trough, Greece

2019 ◽  
Vol 54 (1) ◽  
pp. 34
Author(s):  
Nikolaos Koukouzas ◽  
Pavlos Krassakis ◽  
Petros Koutsovitis ◽  
Christos Karkalis
Keyword(s):  
Plant Material ◽  
Middle Miocene ◽  
Renewable Energy Sources ◽  
Spatial Relation ◽  
Integrated Approach ◽  
Parent Plant ◽  
Sustainable Solutions ◽  
Upper Miocene ◽  
Coal Deposits ◽  
Geological Map

A considerable amount of coal deposits occur within the Mesohellenic Trough in Greece. It is considered as the largest and most important basin of the last orogenic stage of the Hellenides, which is interpreted as a back-arc basin that evolved during the period of Late Oligocene to Miocene. In this study, a simplified geological map has been constructed emphasizing on the coal formation occurrences of the Mesohellenic Trough. This work has been accomplished, through Geographic Information Systems (GIS) and has been organized via geodatabase as GIS data files (feature classes). For the creation of the geological map suitable homogenization and discrete representation has been implemented different geological sheets, original source and traditional maps. Next step was the geostatistical analysis using polygonal methods linked to the corresponding tabular information. Regarding the stratigraphical age, and petrographic data related to geographic distribution of the coal occurrences, these are divided into three categories: Oligocene, Middle Miocene and Upper Miocene coals, exhibiting various physicochemical and topological properties. Upper Miocene coal exhibits the greatest area and perimeter values, while the lowest values correspond to those of the Middle Miocene. Terrain models such as aspect (angle-direction) and hillshade (shaded relief) showed the spatial relation between coal occurrences and morphotectonic as long as geometrical characteristics of the study area. Coals are mainly classified as huminites including mainly huminite group minerals (90%). Their S contents can probably derive from parent plant material or a combination of parent plant material with seawater sulfates. Moisture contents are strongly connected with the sustainability of the coal use in the energy production, while their carbonation grade is strongly associated with their age and expressed by their reflectivity values. All these data have been inserted in an integrated database and can be useful for pre-mining or post mining activities (e.g. planning, analysis, management, restoration). Results of this study are available for the effective evaluation of the existing coal occurrences, which can be used with renewable energy sources providing sustainable solutions, in combination with the upcoming innovative CCS and CCU technologies. Results also showed that coals from the Mesohellenic Trough present excellent quality traits. However, their value as combustible coal is very low due to the absence of economically recoverable reserves. The largest coal lenticular bodies have been extracted in the past and the remaining occurrences do not exceed several thousand tones. Based upon existing literature and from geospatial estimations, coal deposits in the Mesohellenic Trough Basin cannot be considered as economically valuable for exploitation.

AROMATIC BIOMARKER FROM BROWN COAL, SANGATTA COALFIELD, EAST BORNEO OF MIDDLE MIOCENE TO LATE MIOCENE AGE

2016 ◽  
Vol 78 (6) ◽  
Author(s):  
Yulfi Zetra ◽  
Imam B. Sosrowidjojo ◽  
R. Y. Perry Burhan
Keyword(s):  
Aromatic Hydrocarbon ◽  
Organic Compounds ◽  
Brown Coal ◽  
Late Miocene ◽  
Middle Miocene ◽  
Coal Liquefaction ◽  
Low Calorie ◽  
Biomarker Analysis ◽  
Blending Process ◽  
High Calorie

A section of the Sangatta coalfield in the Balikpapan formation located in Kutai Basin, East Borneo, Indonesia, is the Inul area, located North of Pinang Dome. This section of the coalmine has coals with low calories (ca. 4379 cal/g), which is why they cannot be used optimally yet. The reasons of using low calorie coals are besides from being used as a mixing ingredient for the blending process of high calorie coals, they are also used to diversify the coals through the process of coal liquefaction (coal to liquid). In order for the coal liquefaction to be processed correctly, there needs to be a study on the geochemistry organics through coal biomarker analysis, particularly on the hydrocarbon aromatic fractions, so that the origins of the coal organic compounds could be known. Biomarker analysis on the aromatic hydrocarbon fraction shows the existence of naphthalene compound groups with sesquiterpenoids skeleton, phenanthrene with diterpenoids, sesterpenoids skeleton and triterpenoids aromatic pentacyclic. The existence of cadalene compound, triterpene pentacyclic monoaromatic, -triaromatic, -tetraaromatic, -pentaaromatic and triterpenoid C-ring cleaved hydrocarbon with oleanane, ursane and lupane skeletons indicated that the source of coal organic compounds were derived from b-amyrin which were produced by Angiospermae plants. The coal biomarkers distribution, particularly the high abundance of triterpenoid pentacyclic triaromatic compound, confirmed the low maturity of the coals which is predicted to profit from the process of liquefaction due to the high contents of their aromatic fractions.

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.

Middle Miocene fossil grasses from Fort Ternan, Kenya

1993 ◽  
Vol 67 (1) ◽  
pp. 113-128 ◽  
Author(s):  
Daniel P. Dugas ◽  
Gregory J. Retallack
Keyword(s):  
Middle Miocene ◽  
New South ◽  
Single Species ◽  
The United States ◽  
Low Fertility ◽  
Fossil Species ◽  
Southeastern Australia ◽  
South Wales ◽  
Fourth Species ◽  
Dry Woodland

At the well-known fossil mammal locality of Fort Ternan in southwestern Kenya, radiometrically dated at about 14 million years old (middle Miocene), fossil grasses have been preserved by nephelinitic sandstone in place of growth above a brown paleosol (type Onuria clay). Large portions of grass plants as well as fragments of leaves have revealed details of silica bodies, stomates, and other taxonomically important features under the scanning electron microscope. The computer database for grass identification compiled by Leslie Watson and colleagues was used to determine the most similar living grass genera to the five distinct kinds of fossil found. Two of the fossil species are assigned to Cleistochloa kabuyis sp. nov. and C. shipmanae sp. nov. This genus includes one species from low fertility dry woodland soils of New South Wales and Queensland and a second species from “raw clay soils” in western New Guinea. A third fossil species, represented by a large portion of a branching culm, is assigned to Stereochlaena miocenica sp. nov. This genus includes five species of low-fertility woodland soils in southeastern Africa. Both Cleistochloa and Stereochlaena are in the supertribe Panicanae of the subfamily Panicoideae. A fourth species is assigned to Distichlis africana sp. nov. and provides a biogeographic link between the single species of this genus now living in coastal grasslands in southeastern Australia and the 12 species of dunes and deserts found throughout the Americas from Patagonia and the West Indies to the United States and Canada. A fifth species is, like D. africana, in the subfamily Chloridoideae, but its stomata were not seen and it could belong to Cyclostachya, Pogoneura, or Polevansia. This earliest known wooded grassland flora in Africa is taxonomically unlike the modern grass flora of fertile volcanic African landscapes, and may have been recruited from an archaic grass flora of Gondwanan desert and lateritic soils.

scholarly journals Middle Miocene (Badenian) macroinvertebrates from Pécs-Danitzpuszta (Mecsek Mts, SW Hungary)

2021 ◽  
Vol 151 (4) ◽  
pp. 329-334
Author(s):  
Alfréd Dulai ◽  
Tamás Henn ◽  
Krisztina Sebe
Keyword(s):  
Coral Reefs ◽  
Middle Miocene ◽  
Benthic Assemblages ◽  
Brackish Lake ◽  
Lake Pannon ◽  
Central Paratethys ◽  
Upper Miocene ◽  
Marine Deposits

This paper examines Badenian (middle Miocene) macroinvertebrates – corals and molluscs – from the Pécs-Danitzpuszta sand pit (Mecsek Mts, SW Hungary) in order to extend our knowledge on Miocene normal marine deposits of the Mecsek region. Corals occur reworked in the upper Miocene sand that was deposited in the brackish Lake Pannon, and presumably originate either from the middle Badenian Pécsszabolcs or the upper Badenian Rákos Member of the Lajta Formation. A total of seven taxa were identified. These taxa suggest subtropical conditions and a lack of coral reefs in the Badenian. Molluscs were found in situ in the upper Badenian Szilágy Clay Marl Member of the Baden Formation and the Rákos Member of the Lajta Formation. They dominantly consist of bivalves and represent benthic assemblages typical of the middle Miocene Central Paratethys.

scholarly journals The evolution of the fifth cervical vertebrae in Pelomedusoides (Testudines, Pleurodira): a preliminary analysis

2015 ◽  
Author(s):  
Thiago F Mariani ◽  
Pedro S R Romano
Keyword(s):  
Cervical Vertebrae ◽  
Group Discussion ◽  
Neural Spine ◽  
Shape Variation ◽  
Fossil Species ◽  
Ecological Features ◽  
Living Species ◽  
Paraphyletic Group ◽  
Shed Light ◽  
Relative Warps

Background. Crown-Pleurodira (i.e.: Cheloides and Pelomedusoides) possess a side-necked retraction mode with specialized cervical vertebrae (CV) anatomy. Moreover, there are distinctive ecological features among its lineages, as the convergent long neck in species of Chelidae and in the extinct pelomedusoid Araripemydidae. Also, the CV5-CV6 articulation is the major point of flexure in neck retraction and reflects a key point for the evolution of Pleurodira. Here we evaluated CV5 shape variation within some Pleurodira groups with emphasis on some Brazilian fossil species. Methods. We analyzed the fifth CV of eight species and 14 specimens comprising four pleurodiran clades (Chelidae, Araripemydidae, Bothremydidae and Podocnemididae) in order to assess the shape variation via geometric morphometry. All specimens were photographed in caudal view under the same protocol, and eight landmarks (LM) were picked at the left side of each vertebrae using TPSDig2. Data were Procrustes superimposed and a Relative Warps Analysis (RWA) was performed using TPSRelw v1.49. Results. RW1 and RW2 summarized 68.63% of the shape variance. The scatter of the specimens revealed distinctiveness between Podocnemidoidea (Podocnemididae+Bothremydidae) and Araripemys+Chelidae paraphyletic group. Such variation is due to (1) a medial contraction of the surface of the postzygapophysis, (2) a taller neural spine and (3) a more rounded vertebral condile towards Podocnemidoidea. Podocnemididae showed greater variation: a Podocnemis sextuberculata specimen (MZSP3218) is more alike to Cearachelys placidoi (Procrustes Distances, PD=0.17) than other podocnemidids and Bauruemys elegans resembles P. unifilis (PD=0.11). Also, other P. sextuberculata specimen (MZSP3217) is more alike to the Araripemys-Chelidae group. Discussion. Previous works have noticed the anatomical similarities between both longnecked chelids and A. barretoi, considering it as a convergence since they are from different clades. Our data showed the same pattern and, assuming the current phylogenetic relationships of Pleurodira, this might indicates similar feeding behavior between living Hydromedusa and Chelus and Araripemys. The Podocnemidoidea morphospace variation is consistent with the phylogeny, since C. placidoi is nested among Podocnemis spp., and this might indicate a more specialized CV5 for the former and a possible convergence with some Podocnemis species. Also, the resemblance of P. unifilis CV5 with B. elegans seems to indicate a morphotype similar to the podocnemidid ancestor for this living species. Despite our scanty sample, it shows a notable variation in Podocnemis spp. and at least two convergences among CV5 within Pleurodira. Further studies with additional sampling might shed light on a more complex evolution of CV specializations in side-necked turtles than previously assumed.

scholarly journals The biochronology and palaeobiogeography of Baru (Crocodylia: Mekosuchinae) based on new specimens from the Northern Territory and Queensland, Australia

PeerJ ◽  
2017 ◽  
Vol 5 ◽  
pp. e3458 ◽  
Author(s):  
Adam M. Yates
Keyword(s):  
Middle Miocene ◽  
New Records ◽  
Drainage System ◽  
Northern Territory ◽  
Valid Species ◽  
Late Oligocene ◽  
Drainage Basins ◽  
Local Fauna ◽  
The North ◽  
North Western

New records of the Oligo–Miocene mekosuchine crocodylian, Baru, from Queensland and the Northern Territory are described. Baru wickeni and Baru darrowi are accepted as valid species in the genus and their diagnoses are revised. Both species are present in Queensland and the Northern Territory but are restricted in time, with B. wickeni known from the late Oligocene and B. darrowi from the middle Miocene. The broad geographic distributions and restricted time spans of these species indicate that this genus is useful for biochronology. The record of B. wickeni from the Pwerte Marnte Marnte Local Fauna in the Northern Territory establishes that the species inhabited the north-western margin of the Lake Eyre Basin (LEB) drainage system. More southerly Oligo–Miocene sites in the LEB contain only one crocodylian species, Australosuchus clarkae. The Pwerte Marnte Marnte occurrence of B. wickeni indicates that the separation of Baru and Australosuchus did not correspond with the boundaries of drainage basins and that palaeolatitude was a more likely segregating factor.

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