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Sedimentology and Calcareous Nannofossil Biostratigraphy of Alaka Well, Niger Delta, Nigeria 尼日利亚尼日尔三角洲Alaka井沉积学与钙质纳米化石生物地层学
IF 0.9
REVUE DE MICROPALEONTOLOGIE Pub Date : 2021-10-01 DOI: 10.1016/j.revmic.2021.100529
Ndubuisi Ukpabi , Kachikwulu Kingsley Okeke , Mohamed Abioui
{"title":"Sedimentology and Calcareous Nannofossil Biostratigraphy of Alaka Well, Niger Delta, Nigeria","authors":"Ndubuisi Ukpabi ,&nbsp;Kachikwulu Kingsley Okeke ,&nbsp;Mohamed Abioui","doi":"10.1016/j.revmic.2021.100529","DOIUrl":"10.1016/j.revmic.2021.100529","url":null,"abstract":"<div><p><span><span>Calcareous nannofossil<span> biostratigraphy of Alaka well was carried out to identify the biohorizons that exist, ultimately for </span></span>biozonation<span><span><span>, chronostratigraphy and geologic age calibration of the studied interval. The study involved </span>sedimentology<span> analysis, gamma ray description and preparation of two hundred and twelve (212) ditch cuttings, sampled at 9.144m intervals for the study of calcareous nannofossils on smear slides. Sedimentology and gamma ray analyse showed deposition within shallow </span></span>marine paleoenvironments with alternating minor transgressions in a generally progradational delta setting, accounting for the low calcareous nannofossil occurrences. The calcareous nannofossil assemblages recovered from the slide preparations consist of fourteen (14) species, comprising nine (9) long ranged, non-stratigraphic significant forms and five (5) short ranged stratigraphic significant forms. The biohorizons identified included Base (B) occurrence of </span></span><em>Catinaster coalitus</em> at 3578m; <em>Discoaster hamatus</em> at 2874m; Top (T) occurrence of <em>Discoaster hamatus</em> at 2518m and Base absence (Ba) of <em>Reticulofenestra pseudoumbilicus</em> at 2280m. Other biohorizons included Top occurrence (T) of <em>Discoaster bollii</em> at 2435m and <em>Discoaster deflandrei</em> at 3578m respectively. The biohorizons defined boundaries between biozones and showed that the studied interval penetrated four biozones from CNM11 to CNM14 of Backman <em>et al</em><span><span>. (2012), NN7 to NN10 of Martini (1971) and CN5b to CN8a of Okada and Bukry (1980). The geologic age of the studied interval ranged between about 11.60 Ma within CNM11/NN7/CN5b zone to about 8.80 Ma within CNM14/NN10/CN8a zone, the standard chronostratigraphy lies within Tortonian stage. Two chronostratigraphic surfaces were mapped in the studied section and comprised one global maximum transgression at 3514m corresponding to 10.5 Ma maximum </span>flooding event, and one localized maximum transgression at 2847m corresponding to 9.5 Ma maximum flooding surface, separated by sea-level lowstand mapped at 3331m and corresponding to 10.35 Ma.</span></p></div>","PeriodicalId":45442,"journal":{"name":"REVUE DE MICROPALEONTOLOGIE","volume":null,"pages":null},"PeriodicalIF":0.9,"publicationDate":"2021-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.revmic.2021.100529","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"123885978","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Recent ostracods (Crustacea) from the southwestern coast of Peninsular Thailand (Satun Province), Andaman Sea Ostracodes (Crustacea) récents de la côte sud-ouest de la péninsule de Thaïlande (Province de Satun), Mer d'Andaman 最近来自泰国半岛西南海岸(萨通省)的介壳类(甲壳类),安达曼海介壳类(甲壳类)r<s:1> -西部(萨通省)Thaïlande,安达曼海
IF 0.9
REVUE DE MICROPALEONTOLOGIE Pub Date : 2021-10-01 DOI: 10.1016/j.revmic.2021.100526
Marie-Béatrice Forel
{"title":"Recent ostracods (Crustacea) from the southwestern coast of Peninsular Thailand (Satun Province), Andaman Sea Ostracodes (Crustacea) récents de la côte sud-ouest de la péninsule de Thaïlande (Province de Satun), Mer d'Andaman","authors":"Marie-Béatrice Forel","doi":"10.1016/j.revmic.2021.100526","DOIUrl":"10.1016/j.revmic.2021.100526","url":null,"abstract":"<div><p>An inventory of 35 species of ostracods (Crustacea) recovered from sediment samples from a shallow embayment nearby the Mu Koh Phetra National Park in the southwestern coast of Peninsular Thailand, Andaman Sea is given. Most of the species are well-known from the Indo-Pacific area and some others are kept in open nomenclature or compared to already know species because because only few specimens were found. Several species may be new to science but have also to be kept in open nomenclature until new material is obtained. The very abundant specimens of this assemblage are mainly disarticulated valves. This contribution adds to our knowledge of the distribution of ostracods in the Andaman Sea and the degree of ostracod relationship between the Indonesian, Indian and West Pacific areas.</p></div><div><h3>Resumé</h3><p>Un inventaire de 35 espèces d'ostracodes (Crustacea) provenant de sédiments d'une baie peu profonde près du Parc National Mu Koh Phetra sur la côte sud-ouest de la péninsule de Thïlande, Mer d'Andaman, est donné. La plupart des espèces sont bien connues de la zone Indo-Pacifique et certaines sont conservées en nomenclature ouverte ou comparées à des espèces déjà connues en raison du faible nombre de spécimens collectés. Plusieurs espèces semblent nouvelles mais sont aussi conservées en nomenclature ouverte jusqu’à l'observation de nouveau matériel. Les très abondants spécimens qui composent cet assemblage sont principalement des valves désarticulées. Cette contribution accroit notre connaissance de la distribution des ostracodes dans la Mer d'Andaman et de la relation entre les ostracodes des zones indonésiennes, indiennes et ouest-pacifiques.</p></div>","PeriodicalId":45442,"journal":{"name":"REVUE DE MICROPALEONTOLOGIE","volume":null,"pages":null},"PeriodicalIF":0.9,"publicationDate":"2021-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.revmic.2021.100526","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"132581362","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
VSI “Progress on radiolarian research: a selection of studies from InterRad XV, Niigata 2017” VSI“放射虫研究进展:InterRad XV研究选集,新泻2017”
IF 0.9
REVUE DE MICROPALEONTOLOGIE Pub Date : 2021-10-01 DOI: 10.1016/j.revmic.2021.100527
Noritoshi Suzuki , Atsushi Matsuoka , Taniel Danelian
{"title":"VSI “Progress on radiolarian research: a selection of studies from InterRad XV, Niigata 2017”","authors":"Noritoshi Suzuki ,&nbsp;Atsushi Matsuoka ,&nbsp;Taniel Danelian","doi":"10.1016/j.revmic.2021.100527","DOIUrl":"https://doi.org/10.1016/j.revmic.2021.100527","url":null,"abstract":"","PeriodicalId":45442,"journal":{"name":"REVUE DE MICROPALEONTOLOGIE","volume":null,"pages":null},"PeriodicalIF":0.9,"publicationDate":"2021-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.revmic.2021.100527","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"92106139","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
The palynology of the Lower-Middle Jurassic transition of the North Caucasus (southwest Russian Federation), calibrated with index ammonites 北高加索(俄罗斯联邦西南部)中下侏罗统过渡的孢粉学,用指数菊石校正
IF 0.9
REVUE DE MICROPALEONTOLOGIE Pub Date : 2021-10-01 DOI: 10.1016/j.revmic.2021.100517
Аnna A. Goryacheva , Vasily V. Mitta , James B. Riding
{"title":"The palynology of the Lower-Middle Jurassic transition of the North Caucasus (southwest Russian Federation), calibrated with index ammonites","authors":"Аnna A. Goryacheva ,&nbsp;Vasily V. Mitta ,&nbsp;James B. Riding","doi":"10.1016/j.revmic.2021.100517","DOIUrl":"10.1016/j.revmic.2021.100517","url":null,"abstract":"<div><p><span><span><span><span>Palynomorphs from the Toarcian and </span>Aalenian<span> Djigiat Formation of Karachay-Cherkessia in the Kuban River Basin (North Caucasus, southwest Russian Federation) are reported for the first time. Five samples carefully selected for their biostratigraphical content were studied to document the palynological assemblages. Four samples (1, 2, 3, 4) were collected from pieces of rock with key index ammonite specimens, and sample 5 comprises fragments of ammonite shells from a sideritic concretion. Three of these samples (4, 2 and 1) yielded relatively abundant and diverse aquatic </span></span>microplankton (acritarchs, </span>dinoflagellate cysts<span>, prasinophytes and zygnematalean algae) and terrestrial palynomorphs (pollen and spores); the remaining two samples (3 and 5) were less productive and contained fewer than 50 palynomorph specimens. The study of the dinoflagellate assemblages provided characteristic and key information. These are the uppermost Toarcian </span></span><em>Nannoceratopsis</em> Assemblage and the uppermost Toarcian to lowermost Aalenian <em>Parvocysta</em> Suite Assemblage. The former is overwhelmingly dominated by <em>Nannoceratopsis</em> with sparse numbers of the <em>Parvocysta</em> suite, and the latter yielded more diverse and common specimens of <em>Parvocysta</em> and its relatives. This is consistent with the hypothesis that the <em>Parvocysta</em> suite migrated from the Boreal Realm further south into Laurasia during the Toarcian. Certain dinoflagellate cysts such as <em>Mancodinium semitabulatum</em> and <em>Scriniocassis</em> spp., which are typical of Europe and much of Greater Laurasia are absent. Composition of the pollen and spores proved relatively out to be monotonous, and cannot be subdivided. However, in general, the composition of the assemblages of spores and pollen is consistent with the Toarcian–Aalenian transition.</p></div>","PeriodicalId":45442,"journal":{"name":"REVUE DE MICROPALEONTOLOGIE","volume":null,"pages":null},"PeriodicalIF":0.9,"publicationDate":"2021-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.revmic.2021.100517","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122922384","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Dinoflagellate cyst assemblages of the Cunga - Quifangondo cenozoic formations in the Cabo São Brás section, Kwanza Basin (Angola): towards a first stratigraphic and paleoenvironmental interpretation 安哥拉宽扎盆地Cabo s<s:1> o Brás剖面Cunga - Quifangondo新生代组鞭毛藻囊状组合:首次地层和古环境解释
IF 0.9
REVUE DE MICROPALEONTOLOGIE Pub Date : 2021-10-01 DOI: 10.1016/j.revmic.2021.100516
Z. Pereira , M. Mendes , C. Rodrigues , N. Mulanda , M. Cacama , P.C. Nsungani
{"title":"Dinoflagellate cyst assemblages of the Cunga - Quifangondo cenozoic formations in the Cabo São Brás section, Kwanza Basin (Angola): towards a first stratigraphic and paleoenvironmental interpretation","authors":"Z. Pereira ,&nbsp;M. Mendes ,&nbsp;C. Rodrigues ,&nbsp;N. Mulanda ,&nbsp;M. Cacama ,&nbsp;P.C. Nsungani","doi":"10.1016/j.revmic.2021.100516","DOIUrl":"https://doi.org/10.1016/j.revmic.2021.100516","url":null,"abstract":"<div><p><span>This work introduces one of the first palynostatigraphic study conducted on formations from the Eocene and overlying lowermost </span>Miocene successions (Cunga and Quifangondo formations) exposed in the Onshore Kwanza Basin, Angola.</p><p>To improve the Cunga and Quifangondo formations age, new biostratigraphic correlations and palaeoenvironmental interpretations based on qualitative and quantitative analyses of organic walled dinoflagellate cysts from sedimentary rocks sampled in the Cabo de São Brás section were obtained.</p><p>Those works have revealed that the Cunga Formation could be assigned to a middle Eocene - early Oligocene<span><span> age, with a palynomorph signature typical of outer neritic to oceanic environments (dominance of dinocysts with microforaminiferal linings and </span>radiolarian pyritized fragments).</span></p><p>The lower Quifangondo Formation could be assigned to late Oligocene (latest Chattian) - early Miocene (Aquitanian) ages. This assumption is based on the first occurrence of <em>Ectosphaeropsis burdigalensis,</em> and the last occurrence of <em>Deflandrea</em> spp. and <em>Chiropteridium galea.</em> Additionally, the <em>Chiropteridium, Distatodinium, Homotryblium, Hystrichokolpoma</em> and <em>Lingulodinium</em><span> acme endorses a latest Chattian-early Aquitanian age to these samples. The palynomorph signature of this unit reflects an outer neritic environment.</span></p><p>The latest Oligocene/early Miocene Quifangondo Formation overlaps unconformably on strata of the middle Eocene to early Oligocene Cunga Formation, pointing out a hiatus between the two units.</p></div>","PeriodicalId":45442,"journal":{"name":"REVUE DE MICROPALEONTOLOGIE","volume":null,"pages":null},"PeriodicalIF":0.9,"publicationDate":"2021-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.revmic.2021.100516","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"92106138","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
Ostracods like ghosts in their shells: input of X-ray computed tomography for taxonomy and taphonomy of Early Triassic Hollinella 壳子里像鬼一样的介形虫:早三叠纪Hollinella分类和分类的x射线计算机断层扫描输入
IF 0.9
REVUE DE MICROPALEONTOLOGIE Pub Date : 2021-10-01 DOI: 10.1016/j.revmic.2021.100528
Marie-Béatrice Forel , Nathalie Poulet-Crovisier , Lidija Korat
{"title":"Ostracods like ghosts in their shells: input of X-ray computed tomography for taxonomy and taphonomy of Early Triassic Hollinella","authors":"Marie-Béatrice Forel ,&nbsp;Nathalie Poulet-Crovisier ,&nbsp;Lidija Korat","doi":"10.1016/j.revmic.2021.100528","DOIUrl":"10.1016/j.revmic.2021.100528","url":null,"abstract":"<div><p><span>Abundant ostracods of the genus </span><em>Hollinella</em><span><span> (Palaeocopida) have recently been described from the Early Triassic </span>siliciclastic deposits of the paralic Mide B section, Yunnan Province, South China. These weathered and delicate specimens are preserved on the surface of cracked sediments, often still partly buried and impossible to extract. A small piece of siliciclastic sediments with </span><em>Hollinella</em><span> specimens visible on the surface has been investigated by X-ray computed tomography (CT) to search for better preserved and possibly complete specimens still enclosed in the matrix. While surface observations led to the attribution of these specimens to </span><em>Hollinella panxiensis</em> Wang already known from other Permian-Triassic sections in South China, this non-destructive technique reveals distinctive characters that drive us to introduce the new species <em>Hollinella locula</em> Forel nov. sp. Certain previous identifications of <em>Hollinella panxiensis</em> are re-attributed to <em>Hollinella locula</em><span>. The taphonomic analysis of this material is refined and confirms the previous interpretation of a low energy thanatocoenosis. This investigation further highlights the strong implications of new imaging techniques in diverse fields of ostracodology, even in the absence of soft parts preservation.</span></p></div>","PeriodicalId":45442,"journal":{"name":"REVUE DE MICROPALEONTOLOGIE","volume":null,"pages":null},"PeriodicalIF":0.9,"publicationDate":"2021-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.revmic.2021.100528","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"122420340","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Lower Pliocene and Upper Miocene collodarians and spumellarians (polycystine radiolarians) from the northwestern Pacific Ocean (ODP Site 1208) Collodaires et spumellaires (radiolaires polycystines), datant du Pliocène inférieur aux Miocène supérieur de l'océan Pacifique du Nord-Ouest (site ODP 1208) 西北太平洋上新世至中新世下上新世和上中新世胶体和spumellarians (polycystine radiolarians) (ODP位点1208)胶体和spumellarians (polycystine radiolans) (ODP位点1208)
IF 0.9
REVUE DE MICROPALEONTOLOGIE Pub Date : 2021-10-01 DOI: 10.1016/j.revmic.2021.100515
Kenji M. Matsuzaki
{"title":"Lower Pliocene and Upper Miocene collodarians and spumellarians (polycystine radiolarians) from the northwestern Pacific Ocean (ODP Site 1208) Collodaires et spumellaires (radiolaires polycystines), datant du Pliocène inférieur aux Miocène supérieur de l'océan Pacifique du Nord-Ouest (site ODP 1208)","authors":"Kenji M. Matsuzaki","doi":"10.1016/j.revmic.2021.100515","DOIUrl":"10.1016/j.revmic.2021.100515","url":null,"abstract":"<div><p><span>In this study, taxonomic criteria were revised for 64 spumellarians/collodarians from the Upper Miocene<span> that were collected at the Ocean Drilling Program Site 1208. The taxonomic approach employed in this study allowed a relatively wide range of intra-species variation to promote palaeoceanographic studies on Upper Miocene fauna in the future. In addition, the nomenclature of species with controversial taxonomies, for which there is significant biostratigraphic interest, was also revised. One such example is </span></span><em>Stylatractus universus</em> Hays, which should be renamed <em>as Xiphosphaerantha angelina</em><span> (Campbell and Clark). In addition, a new species from the Upper to Middle Miocene core sequences was collected at mid-latitudes of the North Pacific Ocean. This species has been named </span><em>Didymocyrtis noritoshii</em> and can potentially be used as a biostratigraphic and environmental index in core sequences from the Upper Miocene.</p></div><div><h3>Resumé</h3><p>Dans cette étude, les critères taxonomiques de 64 spumellaires et collodaires du Miocène supérieur, collectés sur le site de l'Ocean Drilling Program 1208 sont révisés. Mon approche taxonomique utilisée dans le cadre de cette étude fut libérale, permettant une certaine marge de variations intra-espèces dans le but de promouvoir à l'avenir les études paléocéanographiques en se basant sur la faune radiolaire du Miocène supérieur. En permettant ainsi une plus large variation morphologique au sein d'une espèce, les taxonomies sont plus simples que si on applique une variation morphologique avec des critères assez stricts pour séparer les espèces. En outre, la nomenclature des espèces aux taxonomies controversées parmi lesquelles y figure une espèce à certain intérêt biostratigraphique a également été révisée. C’est le cas de <em>Stylatractus universus</em> Hays, que j'ai renommé <em>Xiphosphaerantha angelina</em> (Campbell et Clark). Enfin, une nouvelle espèce a pu être décrite dans les séquences sédimentaires datant du Miocène supérieur. Cette espèce, qui a été qui fut nommée <em>Didymocyrtis noritoshii</em>, pourrait potentiellement être utilisée comme indicateur biostratigraphique et environnemental dans l'océan Pacifique du nord.</p></div>","PeriodicalId":45442,"journal":{"name":"REVUE DE MICROPALEONTOLOGIE","volume":null,"pages":null},"PeriodicalIF":0.9,"publicationDate":"2021-10-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.revmic.2021.100515","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"130995767","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Radiolaria from the lower Cenomanian (Upper Cretaceous) of Crimea. Part 2. Nassellaria 克里米亚的下盖诺曼尼亚(上白垩纪)的放射虫。第2部分。罩笼虫亚纲
IF 0.9
REVUE DE MICROPALEONTOLOGIE Pub Date : 2021-07-01 DOI: 10.1016/j.revmic.2021.100482
Liubov Bragina, Nikita Bragin
{"title":"Radiolaria from the lower Cenomanian (Upper Cretaceous) of Crimea. Part 2. Nassellaria","authors":"Liubov Bragina,&nbsp;Nikita Bragin","doi":"10.1016/j.revmic.2021.100482","DOIUrl":"10.1016/j.revmic.2021.100482","url":null,"abstract":"<div><p><span><span>Well-preserved Late Cretaceous (early Cenomanian) </span>radiolarians were recovered from two sections in Crimea: Bodrak River and Sel’-Bukhra Mountain. Abundant and diverse Nassellaria were studied and four new species are described: </span><em>Holocryptocanium pseudoastiense</em> nov. sp., <em>Diacanthocapsa bodrakiense</em> nov. sp., <em>Novixitus riedeli</em> nov. sp. and <em>Rhopalosyringium panovi</em> nov. sp. Herein <em>Archaeodictyomitra</em> (?) <em>speciosa</em> Bragina is newly attributed to the genus <em>Obeliscoites</em> O’Dogherty and <em>Dorypyle ovoidea</em> (Squinabol) is tentatively attributed to the genus <em>Homeoarchicorys</em> Empson-Morin. The stratigraphic ranges of <em>Diacanthocapsa urkutica</em> Bragina, <em>Distylocapsa squama</em> O’Dogherty, <em>Novixitus subtilis</em> Bragina, and <em>Siphocampe altamontensis</em><span> (Campbell and Clark) are more precisely defined with their lower limits expanded to the lower Cenomanian and the upper limits of </span><em>Pseudodictyomitra languida</em> O’Dogherty and <em>Thanarla conica</em> (Squinabol) extended to the lower Cenomanian.</p></div>","PeriodicalId":45442,"journal":{"name":"REVUE DE MICROPALEONTOLOGIE","volume":null,"pages":null},"PeriodicalIF":0.9,"publicationDate":"2021-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.revmic.2021.100482","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"134100874","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
Late Messinian ostracods from Eastern Tunisia 突尼斯东部的晚期迈西尼亚介形虫
IF 0.9
REVUE DE MICROPALEONTOLOGIE Pub Date : 2021-07-01 DOI: 10.1016/j.revmic.2020.100467
Francesco Sciuto , Rim Temani , Hayet Khayati Ammar
{"title":"Late Messinian ostracods from Eastern Tunisia","authors":"Francesco Sciuto ,&nbsp;Rim Temani ,&nbsp;Hayet Khayati Ammar","doi":"10.1016/j.revmic.2020.100467","DOIUrl":"10.1016/j.revmic.2020.100467","url":null,"abstract":"<div><p><span>Two stratigraphic sections referable to the late Messinian have been identified and studied in eastern Tunisia; the first, south of Cape Bon (Salakta-SAL section), the second in the Sahel region (Wadi el Kebir–OK section). The analysis of the </span>ostracod fauna content (assemblages) has revealed that in some stratigraphic levels some taxa are certainly attributable to the Lago-Mare fauna, while other taxa, observed in subsequent or previous stratigraphic levels, are referable to true shallow-water marine environments. From these latter shallow water marine levels, several ostracods species were recognized; some of which, due to their morphological particularities, have been described as new species.</p><p>Consequently, in this article, 24 species belonging to the genera <em>Cytherella</em>, <em>Paijenborchellina</em>, <em>Cimbaurila</em>, <em>Pokornyella</em>, <em>Dorukella</em>, <em>Graptocythere</em>, <em>Capsacythere</em>, <em>Chrysocythere</em>, <em>Okadaleberis</em>, <em>Ruggieria</em>, <em>Cytheretta</em>, and <em>Neomonoceratina</em> are described and illustrated as new.</p></div>","PeriodicalId":45442,"journal":{"name":"REVUE DE MICROPALEONTOLOGIE","volume":null,"pages":null},"PeriodicalIF":0.9,"publicationDate":"2021-07-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://sci-hub-pdf.com/10.1016/j.revmic.2020.100467","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"128211767","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 4
BATHYAL OSTRACODS FROM THE UPPER PLEISTOCENE OF THE RIO GRANDE CONE, PELOTAS BASIN, BRAZIL 巴西佩洛塔斯盆地里奥格兰德锥上更新世的深海介形类
IF 0.9
REVUE DE MICROPALEONTOLOGIE Pub Date : 2021-07-01 DOI: 10.1016/j.revmic.2021.100483
Renata Juliana Arruda Maia , Enelise Katia Piovesan , Cristianini Trescastro Bergue , Geise de Santana dos Anjos Zerfass , Robbyson Mendes Melo
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引用次数: 4
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