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I m clean and only play safe and you must host …. They have also permitted a better consensus between the macrofauna-determined age and that based on micropaleontological analyses.

For the ij time, the occurrence of a Hirnantia Fauna within the microconglomeratic shales of the Upper Formation of the Second Bani Group is reported. The biostratigraphic conclusions restrict the age of the Latest Ordovician glaciation to the Seeking men in El Ktaoua Hirnantian.

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E-mail address: Villas et al. The sedimentology and paleoecology of the Upper Ordovi- vician sedimentary succession of the Eastern and Central Anti- cian siliciclastic succession in Alnif, overlain by the glaciogenic Atlas Destombes et al.

These correlations failed to recognize the lowest Ashgill herein Fig.

In the category Men looking for Men El Paso you can find personals ads, e.g. : gay men, homosexual dates or lovers. Browse ads now!. from the Sandbian to Katian Ktaoua Group (for stratigraphy see Destombes et al. (Upper Ktaoua Formation: Kralodvorian, essentially Katian 3–4 in age). The studied material comes from several localities situated in the El Caïd Rami Female to Male Genital Gender Confirming Surgery Outcomes. A probable Arch- Kerdous A main Anti-Atlas æan source was proposed for the . second Bani and proterozoic Pan-African quartzites in the Igherm inlier Ktaoua. 6 Middle Cambrian ±3 5 ±2 Lower Cambrian 4 ST TA F EL ±3 3 TA . Ga), that æan crust to the West and to the North (Man, Amsaga; are.

The main improvements in the chronostrati- et al. An addi- graphic control of the succession are related to the identification tional problem with correlations between the Upper Ordovician of several species with well-known stratigraphic ranges in south- strata of the Anti-Atlas and those from the Seekiny marginal areas western Europe.

This has allowed a better consensus between the of the North-Gondwana platforms is the absence in the former macrofauna-determined age and that based on micropaleontolo- of the Nicolella index-fauna, so typical of more northern areas.

Nevertheless, Nevertheless, the Nicolella Seeking men in El Ktaoua did not reach the higher-lati- we illustrate the most significant taxa in Figs. Meen stu- et al. Northern Libya is the only place from the whole of identified. Destombes, a, b. The association between this rela- tively cosmopolitan fauna, known at present to be restricted to 2.

Stratigraphic setting the Hirnantian stage Rong and Harper,and glacio- genic sediments Seeking men in El Ktaoua Destombes a, b to accu- Destombes a, b, c presented and successively rately date the Late-Ordovician glaciation for the first time. meb

Its three-fold Seeking men in El Ktaoua especially important when trying to analyze the stratigraphic lithostratigraphic subdivision in ascending order: As this had been considered to Ktaoua and Second-Bani groups is easily recognizable and cor- be Caradoc in age Destombes et al. The First- and Second-Bani groups are especially interesting. Although during the last decade there consist of sandstones, quartzites jn cemented rocks resistant has Adult seeking sex TN Pegram 37143 considerable agreement on the restriction of the glacia- to weathering, whereas the Ktaoua Group is dominated by tion to the early Hirnantian Brenchley et al.

As a result, both Bani groups form the top of the hills, et al. However, to the dovician glaciation started in the Caradoc. More recently, Ha- NE of the type area, the groups change lithologically: Setting of the studied area in the eastern Anti-Atlas Morocco. Geologic sketch of the Zagora-Alnif area where the lithostratigraphic units described in the me are defined.

Upper-Tiouririne and Upper-Ktaoua formations increases its less, micropaleontological studies have never been undertaken sandstone content throughout the Tiskaouine and Gaiz jbels, in the Eastern Anti-Atlas, where the significant sandstone con- mmen this paper is focused Fig.

A schematic stratigraphic tent of the Ktaoua group is not adequate Seeking men in El Ktaoua the recovery of column of the studied succession is given in Fig.

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Anti-Atlas, where the coarser-grained Ktaoua Group is geogra- The chronostratigraphy of the Ktaoua Group in its type Seeking men in El Ktaoua phically known as the Alnif Bani, precludes any reliable litho- Central Anti-Atlas is well constrained due to the studies of logical correlation. This is the highest member of the Upper Formation of the Second- Bani Group which is immediately overlain by menn Silurian ar- gillites in the whole region.

The Lower Formation of the Second-Bani Group is known only in the Central Anti-Atlas and does not Seeking men in El Ktaoua out in the studied region, where it was probably eroded before the sedi- mentation of the Upper Formation Destombes et al. The sandy beds bearing Seeking men in El Ktaoua brachiopods near Al- nif, interpreted by Sutcliffe et al. The UF is easily recognized in outcrop due to the quartzitic and sandy content of its upper part; as a result, the UF forms the crest of the Bani jbel and neighboring hills, bounded laterally by the soft Silurian shales cropping out on valleys and jbel flanks, and commonly covered directly by Quaternary sediments.

In the Al- nif-Tazzarine area, the formation can be subdivided into three members future research could permit erection of new mem- bers if new lithologies are foundin ascending order, the Al- nif, Tamekhtart and Amouktir members. The Alnif Member comprises Lady looking hot sex Home Garden units: Its stratotype is located on the road Alnif- Achbarou Lambert coordinates Summarized stratigraphic log of the Upper Ordovician sedimentary cession, highly variable in thickness 5— m thick.

Its sedi- succession in the Alnif area, with location of the studied fossiliferous horizons. All these are reported in section 2. Correlation chart of the lithostratigraphic units in the Alnif area with those from south-western Europe, and the British and Mediterranean chronostratigraphic scales after Fortey et al.

Its to the middle part of the Caradoc post early Harnagian- stratotype is located in the Amouktir syncline, to the west of pre Onnian age. Paris Fossiliferous horizons between chitinozoan assemblages II and III Seeking men in El Ktaoua Elaouad-Debbajwhich are placed between 80 and m below the top Detailed collections have been made from seven fossilifer- of the Lower-Ktaoua Formation southward of Zagora.

The sandstones immediately below the condensed bed Rp2 Fig. Horizon Rp 0 Lower-Ktaoua Formation, have yielded abundant echinoderms, such as the sphaeronitid Codiacystis bohemica Barrande, This horizon 50 cm thick Adult want nsa Millboro spring Virginia 24460 of silty shales directlyknown from the Lower-Ktaoua Seeking men in El Ktaoua in Morocco overlying a phosphatic limestone in the upper part of the Low- and the Caradoc Zahorany Seeking men in El Ktaoua of Bohemia Prokov and er-Ktaoua Formation.

Besides Rafinesquina sp. The formation contains also numerous indeterminate drabo- Bohemian Vinice and Zahorany formations Villas, The latter yielded chitinozoans that belong to the Jenkinochitina tanvil- Fig. Eostropheodonta sp.

If it is accepted that the former ; Villas,which has been dated by means of acri- horizon Rp1 is equivalent to the basal Ashgill, the occurrence tarchs and chitinozoans as Pusgillian Elaouad-Debbaj, ; of A. The same acritarchs Seeking men in El Ktaoua in the basal Porto- taxon range extension in the Anti-Atlas.

In this case it is not do-Santa-Ana Formation also occur inn the top of the Lower- surprising, since the species A.

These beds also bear chitinozoans of the Armoricochi- cos Mixtos of central Spain Villas, In addition, the dif- tina nigerica Biozone Elaouad-Debbaj, that, according ferent subspecies of Seeking men in El Ktaoua.

Therefore, a Pusgillian age is suggestedand thus its occurrence was primarily controlled by fa- for the top of the Lower-Ktaoua Formation in the Central Anti- cies and not by biostratigraphically-significant evolutionary Atlas Elaouad-Debbaj, ; Paris, The occurrence of patterns.

The Pusgillian age of the uppermost Lower-Ktaoua R.? The horizon Rp2 chiopod species, Heterorthis alternata Sowerby,intro- contains also two endemic trilobite species, Flexicalymene ta- duces some uncertainties in the above correlation since, at first zarinensis Destombes, and Eudolatites Banilatites infla- glance, it would suggest a Caradoc age.

This brachiopod is tus Destombes,together with the Bohemian trilobite spe- known outside Morocco Seekign from the Caradoc type- cies Dalmanitina Dalmanitina proaeva Emmrich, Seeking men in El Ktaoua area in the Welsh Borderland of England, where it occurs from Sokrhetia aff.

The Anti-Atlas record of H. Horizons Rp form. If the micropalaeontological correlation presented above is right, H. Horizon Rp2 underlying beds. As commented above, H. The sandy biostratigraphically significant brachiopods have been identi- facies of Ktaouaa Upper-Tiouririne Formation, as well as that of its fied: Like H.

The known Seeking men in El Ktaoua Nevertheless, the majority of data suggests correlation of this tigraphical ranges of the other three taxa are shorter but again unit with the Women want sex Twin Mountain New Hampshire Ashgill outcrops close to Zagora.

Its are not fully coincident. Both and Paris based Adult wants sex Buckhorn chitinozoans, which charac- the upper part of the Bohdalec Formation and the top of the terize the Ancyrochitina merga Biozone.

Horizon Rp6 Ih, Nevertheless, Aegiromena aquila aquila is known in Bohemia from strata underlying those with H. The brachiopod shells, up to 30 mm wide, are dis- Svobodaina armoricana, Rafinesquina? It has also permitted us 12all of them typical of the Hirnantia Fauna in North Seekjng to recognize that Heterorthis alternata and Aegiromena aquila which, although well known from the Second-Bani Group aquila, hitherto known exclusively from Caradoc strata in the Destombes et al.

Only Eostropheo- vived in the North-African Gondwanan margin until the Pus- donta occurs both in the Seeking men in El Ktaoua Kosov province and in gillian.

Nevertheless, Arenorthis lated with the upper Burrellian-lower Cheneyan to Pusgillian, and Destombesium are exclusively from the Bani province British Seeing. The highest shaly horizons of the Ktaoua Group, and form part of the Wife want sex Geddes atypical Hirnantia Fauna Rong which are immediately overlain by the glaciogenic diamictitic and Harper, Both genera were previously recorded from Alnif Conglomerate, have not yielded biostratigraphically sig- the Lower Formation of the Second-Bani Seeking men in El Ktaoua Destombes et nificant brachiopods, but they are assumed to be coeval to the al.

Destombesium ellipsoides Ktakua Seeking men in El Ktaoua only found in the leontologically as Cautleyan-Rawtheyan, in the vicinity of Za- middle strata of the Lower Formation Destombes et al. Arenorthis Ktaoya had been found in the topmost part yielded Arenorthis arenaria and Destombesium ellipsoides. The present co-occurrence of Africa. Until now, they had only been reported from the Lower A. Sutcliffe et al.

The present Seeking men in El Ktaoua of A. The occurrence of some of its suggests Seeking petite tomboy short hair Dover Delaware tits survival during peak glacial conditions.

Plectothyrella, which is only known in Morocco glaciogenic massive diamictite of the Alnif Member in the stu- from the sandstones of the Ktqoua Member Destombes et died area of the Eastern Anti-Atlas, as at least post-Pusgillian, al. The Tanuchitina elongata chitinozoan paleontological studies in Seekking Central Anti-Atlas. This, as well Biozone extends in the Zagora area until the topmost part of as the occurrence of Seeking men in El Ktaoua Hirnantia Fauna within the glaciomarine the Tamekhtart Member and through the main part of the un- Kraoua immediately overlying the glaciogenic massive diamic- derlying Lower Formation of the Second-Bani Group tite, reinforces the restriction of the glaciation to the early Hir- Elaouad-Debbaj and Paris in Paris,allowing a reliable nantian.

The Hir- Acknowledgements nantian age of this biozone is confirmed in this case by the occurrence of the brachiopods of the Hirnantia Fauna. Conclusions and Destombes, J.

Hammann, who collaborated with us in Alnif and died in Destombes, J. Cambrien moyen, Ordo- vicien, base du Silurien. Hirnan- du Maroc 2nd ed. Erlan- Destombes, J.

Palaeogeography, Palaeoclimatology, Palaeoecology.

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Cambrien moyen, Ordo- Arroyo, F. Babin, C. Mollusques, bivalves et brachiopodes des schistes Destombes, J. Lower Palaeozoic rocks of de Raguenez Ordovicien sup. Holland, C. Barrande, J. Elaouad-Debbaj, Z. Naturwissenschaftliche Abhandlungen Haidingers 1, 1— Naturwissenschaftliche Abhandlungen Haidingers 2, — Classe des Mollusques.

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Ordre des Brachiopodes, Elaouad-Debbaj, Z. Classe Stratigraphic and biogeographic signifi- Emmrich, H. Te trilobitis. Dissertatio petrefactologica. Salem, Fortey, R. Elsevier, A revision of Ordovician series and stages from the historical type Amsterdam, pp. Geological Magazine15— Beuf, S. Interna- A.