What is Nummulites depressus Kenawy 1978? Evolution of Nummulites fabianii group in the Middle Eocene of Egypt

New species Nummulites vetustufabianiin. sp. is described from the El Hamra Formation, Gara El Hamra section Bahariya Oasis Western Desert. The biometrical measurements include maximum and minimum diameter of the successive radii and heights of whorls, length/height ratio, number of chambers and the marginal cord thickness of each whorl for the megalospheric generation as well as the diameter of proloculus were elaborated to differentiate between some allied granulated species such as Nummulites depressus, Nummulites decrouezae, Nummulites cuvillieri and N. vetustufabianiin. sp.Nummulites fabianii group has lateral distribution for the entire Tethys basin, hence such biometrical studies are needed to emphasise the polyphyletic nature of the group.     

New Middle Eocene Nummulites from Kait Bey,Gebel Mokattam,Egypt

Nummulites paucispira and Nummulites kaitbeyi are newly erected from the Upper Building Stone Member (Bartonian) of the Mokattam Formation at Kait Bey, Gebel Mokattam, Greater Cairo, Egypt both belong to Nummulites partschi group. N. paucispira and N. kaitbeyi are different in their ontogenetic growth stages; N. paucispira has a step of coiling from tight to lax, contrary to N. kaitbeyi. The regression line of both species indicates that both are distinct and they belong to different lineages. Detailed investigations of the new species N. paucispira n. sp. and N. kaitbeyi n. sp. of N. partschi group and their ontogenetic growth stages are discussed. This study is of considerable importance for distinguishing paleoecological events of Bartonian stage and for tracing the phylogenetic trends for the entire Tethys basin.     

Microbial maceration and carbonate dissolution on cold‐temperate shelves

Nummulites beaumonti d'Archiac & Haime, 1853, originally described from El Basatin, Gebel Mokattam, Greater Cairo, is redefined from a nummulitic bank at the base of the Maadi Formation from its type locality as neotype. Schaub (1981) described the species from Libya and the type example of this species is still unknown. N. discorbinus Schlotheim (1820) is described as neotype from a nummulitic bank in the Mokattam Formation, which is located in the site of the Citadel tombs, near the Salah El Din Citadel, Gebel Mokattam, Egypt. According to Schaub (1981), the type example of this species is also unknown. For this reason the establishment of the neotypes of these two widespread nummulites species: N. discorbinus (Late Lutetian) and N. beaumonti (Bartonian) is important and tackled in this paper. N. qurnensis n. sp. ( = N. sp. cf. beaumonti in Boukhary et al. 2002) is introduced as a new species from the lower Bartonian part of the Qurn Formation of Helwan. Biometrical studies are carried out on the three species to present up to date information on these Nummulites, with particular attention to their biostratigraphic correlation with the Shallow Benthic Zones (SBZ) of Serra-Kiel et al. 1998. The authors would like to stress the importance of a careful designation of a neotype to avoid the introduction of complicated and unnecessary taxonomic problems.     

New larger foraminifers from the Eocene of the Crimea (Ukraine) and Mangyshlak (Western Kazakhstan)

Two new species of Nummulites and one subspecies of Orbitoclypeus from the Eocene of the Crimean Mountains and Mangyshlak Peninsula are described in detail. Nummulites alexisi sp. nov. and Orbitoclypeus munieri major subsp. nov. come from the Upper Ypresian, while Nummulites ninikae sp. nov. is from the Lower-Middle Lutetian. The phylogenetic position of new taxa is discussed.     

Middle-upper Eocene ostracods and nummulites from Gebel Na’alun, southeastern Fayum, Egypt

The middle-upper Eocene sequence at Gebel Na’alun, southeastern Fayum yielded 21 ostracod and four nummulite species. Out of these, two new ostracod species namely Bairdia crolifai and Paracypris naalunensis are described. Four ostracod assemblages are distinguishable; the lower three are assigned to the Bartonian and the upper one is Priabonian. The nummulites exist in three stratigraphic horizons represented from base to top by “Nummulites” aff. pulchellus, Nummulites decrouezae with Nummulites cavelieri (Bartonian) and Nummulites aff. fabianii (Priabonian).     

A new species of Neochelys (Chelonii,Podocnemididae) from the Ypresian (Early Eocene) of the South of France

The known European record of the Gondwanan group Podocnemididae begins in the Early Eocene. Neochelys underwent a rapid diversification and was an abundant and diverse representative of this group during the Eocene of Europe from the Early Ypresian to at least the Bartonian. However, several of its species are poorly known, and the phylogenetic relationships among them are poorly understood. A complete shell from the Ypresian of Hérault (southern France) is described here. It is assigned to a new species, Neochelys liriae. The availability of characters of N. liriae is tested by comparison with the other European species, which appear to be well differentiated, and particularly with the neighbouring French taxa N. eocaenica and N. laurenti, of which the latter has been little known to this point.     

Middle–Late Eocene Nummulites (N. burdigalensis group) from Gebel Hafit,along the United Arab Emirates and Oman borders,Arabian Peninsula

A Middle–Late Eocene diagnostic larger foraminiferal assemblage is described and illustrated from carbonates of the uppermost Dammam Formation, on both sides of Gebel Hafit anticline in the Northern Oman Mountains in the United Arab Emirates. The Middle Eocene carbonates yielded Nummulites obesus d'Archiac, 1852, N. ismaili Boukhary, Hamdan & Bahr n. sp., N. papazzonii Boukhary, Hamdan & Bahr n. sp. and N. kenawyi Boukhary, Hamdan & Bahr n. sp. (a species of the N. burdigalensis group). In addition, N. cf. boussaci Rozlozsnik, 1924, N. cf. lorioli De La Harpe, 1879, N. hottingeri Schaub, 1981, N. strougoi Boukhary, Hamdan & Bahr n. sp. (of the N. partschi group), N. ansaryi Boukhary, Hamdan & Bahr n. sp. (of the N. gizehensis group), N. cf. praebullatus Schaub, 1981, N. cizancourti Sander, 1962 (of the group of N. fabianii), N. cf. stamineus Nuttall, 1927 (of the N. discorbinus group), N. maculatus Nuttall, 1926 (of the N. laevigatus group) and Assilina gigantea De La Harpe, 1926 are recorded. On the top of the sequence, an assemblage with N. hottingeri Schaub, 1981, which was assigned by Schaub 1981 to the Biarritzian ( = Bartonian), was found associated with N. ptukhiani, Silvestriella tetraedra (Gümbel, 1870) and Pellatispira madaraszi (Hantken, 1875); these findings suggest that this association should be assigned to the Priabonian stage, confirming for the sampled succession of a Late Eocene age for sediments deposited in an inner-shelf environment, which was possibly related to the eustatic fall of sea level at the end of the Priabonian.

http://zoobank.org/2EBD2891-293F-465A-AE1C-F419F0CDB970     

Oligocene larger foraminifera from United Arab Emirates,Oman and Western Desert of Egypt

An early Oligocene (Rupelian) diagnostic larger foraminiferal assemblage is described and illustrated from marls and limestones of the Asmari Formation, at Jabals Hafit and Malaqet in the UAE. An equivalent assemblage is identified in the mudstones of the Tahwah Formation, Wadi Suq, Oman. Although Nummulites intermedius (D'Archiac 1846) and N. fichteli are fully synonymous (e.g. Roveda 1970; Schaub 1981; Sirel 2003), in this study both species are biometrically differentiated, distinct and both names are valid. N. fichteli Michelotti 1841, N. intermedius (D'Archiac 1846) and N. emiratus n. sp., which are index for the early Oligocene (Rupelian), and they are replacing each others competitively and environmentally.

The presence of Blondeauina bouillei n.gen., N. emiratus n.sp., N. intermedius, N. fichteli, Planoperculina complanata (Defrance 1822) and Austrotrillina asmariensis Adams 1968 ascribed the section of the Asmari Formation to the early Oligocene (Rupelian). The studied marls and limestones were deposited in outer and inner shelf environments, respectively. The Asmari Formation in the area studied consists mainly of marl in its lower portion and reefal limestone in its upper part, indicating a major marine regression. The Tahwah Formation in Oman is composed of bioturbated silty and muddy marls and is a facies equivalent to the Asmari Formation marls. The Asmari Formation facies change probably relates to a mid-Oligocene fall in global sea level.

In this study, the Dabaa Formation, a subsurface unit of late Eocene–Oligocene marine shales in the north Western Desert of Egypt, was chosen to correlate with the Oligocene of Emirates and Oman. The Dabaa Formation comprises Spiroclypeus ornatus (Henson 1937) and Eulepidina dilatata (Michelotti 1861). The environment of deposition was inner shelf to littoral, which become estuarine towards the top in many areas. This Oligocene Dabaa sequence is correlatable with Wadi El Arish sequence recently discovered by Kuss and Boukhary (2008) from Risan Aneiza, Northern Sinai, Egypt.     

L’emploi des méthodes de la théorie des ensembles flous à l’étude biométrique de l’espèce Nummulites millecaput dans la partie occidentale de la Téthys

Application of the fuzzy set theory to the biometric evaluation of the species Nummulites millecaput in the western part of the Tethys. The goal of this paper is to demonstrate the ability of the fuzzy-set theory to contribute to the evaluation of paleontological problems. As an example, the species Nummulites millecaput, Boubée has been chosen. One hundred specimens of this species, collected from four localities (Arrimblar, Adelholzen, Dudar, and Mount-Kotuc) have been prepared (equatorial sections) for the biometric measurement of the external and internal characteristics. First a traditional statistical evaluation was performed, followed by the construction of membership functions, the latter ones expressing in the best way the transitions from one locality to the other. The results of this evaluation confirmed that from Aquitaine (France) to Armenia, the same species – Nummulites millecaput – was distributed during the Eocene. To cite this article: G. Bárdossy et al., C. R. Palevol 2 (2003).     

Heliorestis convoluta sp. nov., a coiled, alkaliphilic heliobacterium from the Wadi El Natroun, Egypt

A morphologically distinct heliobacterium, strain HH, was isolated from Lake El Hamra, a soda lake in the Wadi El Natroun region of northwest Egypt. Strain HH consisted of ring-shaped cells that remained attached after cell division to yield coils of various lengths. Strain HH showed several of the physiological properties of known heliobacteria and grouped in the Heliorestis clade by virtue of its phylogeny and alkaliphily. The closest relative of strain HH was the filamentous alkaliphilic heliobacterium Heliorestis daurensis. However, genomic DNA:DNA hybridization results clearly indicated that strain HH was a distinct species of Heliorestis. Based on its unique phenotypic and genetic properties we describe strain HH here as a new species of the genus Heliorestis, H. convoluta sp. nov.Dedicated to Prof. Dr. Norbert Pfennig on the occasion of his 80th birthday.     

Larger benthic foraminiferal assemblages and their response to Middle Eocene Climate Optimum in the Kohat Basin (Pakistan,eastern Tethys)

The Middle Eocene Climatic Optimum (MECO) at ～40 Ma is a significant global warming event associated with pronounced changes in the hydrosphere, atmosphere, and biosphere. The Kohat Formation in the Kohat Basin (eastern Tethys, Pakistan) is studied for identifying the response of larger benthic foraminifera (LBF) to MECO. The LBF assemblages in the Kohat Formation, covering from the Shallow Benthic Zones (SBZ) 15 to 17, suggest middle Lutetian to early Bartonian in age. Microfacies analyses indicate a lagoonal (inner carbonate ramp facies belt) to open marine (middle carbonate ramp facies belt) paleodepositional environment of the Kohat Formation. A distinct positive δ¹³C shift marks the stratigraphic position of the MECO in this formation. At the Peak-MECO event that is marked by the onset of the positive carbon isotope excursion (CIE), no evident compositional variation in the LBF assemblages is observed. However, significant changes in the LBF assemblages with the local first and last occurrences of some LBF genera can be observed in the Post-MECO and CIE recovery phase. These changes are verified by the sudden disappearance of Alveolina and orthophragminids and initial dominance of larger shell-size Nummulites fabianii, Heterostegina, and Linderina species accompanied by an increase in the species diversity. Here, we argue that the change in the observed LBF assemblages in the uppermost part of the Kohat Formation might be related to a larger foraminiferal turnover occurring during the Post-MECO event and corresponds to the CIE recovery phase.     

Intraindividual variability in Sinonamuropteridae forewing venation (Grylloblattida; Late Carboniferous): taxonomic and nomenclatural implications

The family Sinonamuropteridae has been erected for nine fossil insect species from the Late Carboniferous Tupo Formation (Ningxia, China), each represented by a single isolated forewing. The family has been assigned to the order Diaphanopterodea (extinct palaeopteran order). We investigated the forewing venation pattern and its variability in this family based on an abundant collection from the same locality. Based on new data on Chelopterum peregrinum Carpenter, 1950 (Grylloblattida; Lower Permian; Wellington Formation, U.S.A.) and the new material, we demonstrate that the nine sinonamuropteridaean species form a single one: Sinonamuropteris ningxiaensis Peng et al., 2005 . The following genera are considered as synonyms of Sinonamuropteris: Separatonerva Peng et al., 2005 syn.n. , Combonerva Peng et al., 2005 syn.n. and Tectonerva Peng et al., 2005 syn.n. The following species (all with Peng et al., 2005 , as their authority) are considered as synonyms of S. ningxiaensis: Separatonerva longa syn.n. , Separatonerva qilianshanensis syn.n. , Combonerva granulata syn.n. , Combonerva huangheensis syn.n. , Tectonerva longovata syn.n. , Sinonamuropsis zhongweiensis syn.n. , Sinonamuropsis rugoverrucosa syn.n. , Sinonamuropsis xiaheyanensis syn.n. The family must be assigned to the neopteran order Grylloblattida.     

First record of the extinct sawfish <Emphasis Type="Italic">Propristis schweinfurthi</Emphasis> Dames, 1883 (Batoidea: Pristiformes: Pristidae) from the middle Eocene of Spain

A partial rostrum of Propristis schweinfurthi Dames, 1883 was collected in the Bartonian strata of northeastern Spain. The specimen represents the second record of the species from Europe, and the second occurrence of a sawfish (Mesopristis osonensis Farrés, 2003) from the Vic-Manlleu Marls Formation. In spite of some evidence to the contrary, Propristis probably preferred ecological conditions similar to extant sawfishes, i.e., inhabiting nearshore tropical to subtropical seas with occasional excursions into freshwater.     

A triassic “Problematic microfossil” revealed:<Emphasis Type="Italic">Probolocuspis espahkensis</Emphasis> Brönnimann,Zaninetti, Moshtaghian and Huber 1974 is attributed to the dasycladacean algae

Summary The “problematic microfossil”Probolocuspis espahkensis, described as, “incertae sedis” by Br?nnimann, Zaninetti, Moshtaghian and Huber (1974) from the Carnian Espahk Formation near the small village of Espahk (Tabas area, NE Iran) represents a dasycladacean alga attributed preliminary to the Family Acetabulariaceae, Tribe Clypeineae. The holotype ofProbolocuspis espahkensis, designated by Br?nnimann et al. (1974), is only a part of the alga. Contribution to the Triassic Paleontology of Iran No. 8; for No. 7: see Senowbari-Daryan, B. (2002); Jb. Geol. Bundesanst., 143/I, Wien     

Bio- and sequence stratigraphy and microfacies analysis of the Oligocene Asmari Formation at Sepidar Anticline,Interior Fars sub-Basin,SW Iran

In this research, biostratigraphy, microfacies analysis and sequence stratigraphic framework of the Asmari Formation are discussed at Sepidar Anticline, Interior Fars sub-Basin. The strata are Rupelian to Chattian in age. According to the distribution of benthic foraminifera, two assemblage zones were recognised (I-) Nummulites vascus–Nummulites fichteli and (II-) Archaias asmaricus/hensoni–Miogypsinoides complanatus. Eight microfacies types which can be grouped into three depositional environments are recognised. Distribution of Oligocene foraminifera together with other constituents allowed the identification of three third-order sequences at Asmari Formation. Correlation of analysed sections through Interior Fars sub-Basin represents the development of a carbonate ramp with a deepening trend from SE to NW along the Rupelian/Chattian boundary.     

Length–weight relationships of five fish species collected from Basistha River,a torrential river in Assam,India

Length–weight relationships (LWRs) are presented for five species, namely: Garra nasuta (McClelland, 1838); Garra gotyla gotyla (Gray, 1830); Devario aequipinnatus (McClelland, 1839); Barilius bendelisis (Hamilton, 1807) and Pseudolaguvia shawi (Hora, 1921) collected from the Basistha River, Guwahati, Assam, India. Information regarding LWR data for four of these species was not yet available in FishBase (Version 04/2015; Froese and Pauly, 2015).     

A new species of Tardigrada (Eutardigrada: Milnesiidae): Milnesium krzysztofi from Costa Rica (Central America)

Abstract

A new eutardigrade species Milnesium krzysztofi sp. nov. is described from Costa Rica. M. krzysztofi sp. nov. differs from the most similar Milnesium katarzynae Kaczmarek et al., 2004 mainly by the presence of spurs on internal claws I–III and on external claw IV.     

New Middle Permian insects from Salagou Formation of the Lodève Basin in southern France (Insecta: Pterygota)

Summary

New insects are described from the Middle Permian (Guadalupian) of Salagou Formation in the Lodève Basin (Languedoc region, France). Palaeopterans are represented by new odonatopterans viz. Huangiopterum lodevense n. gen., n. sp. and Huangiopterum species B, attributed to clade Panodonata (Huangiopteridae n. fam.), already recorded through the family Saxonagrionidae in the same formation, and a diaphanopterodean Martynovia cf. halli Beckemeyer 2004 (Martynoviidae) known from the Lower Permian of Oklahoma. Archaeorthopterans are supplemented by Bethouxia ariegensis n. gen., n. sp., Paralongzhua elongata n. gen., n. sp., Lodevolongzhua incompleta n. gen., n. sp., the caloneurodean Jarmiloptera mouralensis n. gen., n. sp., and a cnemidolestodean cf. Tococladus sp. (Tococladidae). Permophyllum rotundatum n. sp. (?Tettigoniidae) demonstrates the first presence of Orthoptera with wings probably mimicking Peltaspermales reproductive organs in Late Palaeozoic possibly analogous to the known crypsis of roachoid tegmina with pteridosperm pinnules. Frequent occurrence of hardly identifiable grylloblattid wing fragments support their significant role in term of abundance and diversity of the Permian faunas. New taxa based on wing venation pattern as Genera and species undetermined A, B (Liomopteridae), Permobaharellus salagousensis n. gen., n. sp. (family uncertain), Lodevophlebia reticulata n. gen., n. sp. (Sylvaphlebiidae), Oborella lodevensis n. sp. (Euryptilonidae), and Genus and species undetermined C, were described. Paoliida is represented by a paoliid gen. et sp. indet. and three anthracoptilids Strephocladus gandi n. sp., Strephocladus mouralensis n. sp., Lodevocladus subtilis n. gen., n. sp. The first record of miomopteran Palaeomantis sp. (Paleomanteidae) from Salagou Formation is presented. Acercarian insects are represented by the first record of Thripida and diverse new hemipterans, namely Euroscytina lutevanorum n. gen., n. sp. (Cicadomorpha: Scytinopteridae), Prosbole dio n. sp., Prosbole garrici n. sp., Pervestigia cf. veteris Becker-Migdisova 1961 (Prosbolidae), Archescytina species A (Paleorrhyncha: Archescytinidae) and Permopsyllidium lesclansis n. sp. (Sternorrhyncha: Psylloidea: Protopsyllidiidae). Entomofauna from the Salagou Formation demonstrate highly diverse insect communities with some taxa linked to early and late Permian ones known from assemblages in Euramerica and Russia, such as Obora (Czech Republic), Wellington Formation (Kansas and Oklahoma, USA), and Tshekarda (Ural, Russia).     

山西垣曲盆地始新世轮藻植物群

记述山西垣曲盆地河堤组任村至寨组里段轮藻化石,计１１属,１４种,２未定种,建立了一个地区性轮藻化石组合：Ｒａｓｋｙｅｌｌａｓｉｎｅｎｓｉｓ－Ｌｉｎｙｉｅｃｈａｒａｄｅｃｏｒｏｓａ－Ｓｔｅｐｈａｎｏｃｈａｒａｇｌｏｂｕｌａ组合,该组合位于中国早第三纪轮藻植物群序列中Ｏｂｔｕｓｏｃｈａｒａｊｉａｎｇｌｉｎｇｅｎｓｉｓ－Ｇｙｒｏｇｏｎａｑｉａｎｊｉａｎｇｉｃａ植物群的上部,轮藻植物群反映的地质时代始新世