Micropaleontology最新文献

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Oxfordian Benthic Foraminifera and Ostracods from the Hanifa Formation (Hawtah Member), Central Saudi Arabia 沙特阿拉伯中部哈尼法组(Hawtah组)牛津底栖有孔虫和介形类
IF 1.5 4区 地球科学
Micropaleontology Pub Date : 2021-01-01 DOI: 10.47894/mpal.67.6.04
Saleh S. Aba Alkhayl
{"title":"Oxfordian Benthic Foraminifera and Ostracods from the Hanifa Formation (Hawtah Member), Central Saudi Arabia","authors":"Saleh S. Aba Alkhayl","doi":"10.47894/mpal.67.6.04","DOIUrl":"https://doi.org/10.47894/mpal.67.6.04","url":null,"abstract":"The Hanifa Formation in Saudi Arabia consists of mostly carbonate units of Late Jurassic age and is well exposed along the Tuwaiq Mountain escarpment. Micropaleontological analyses of samples from three outcrops have revealed the presence of benthic foraminifera and ostracods. The study of fossil faunas from the Hawtah Member, has led to the identification of six foraminiferal species: Alveosepta (Redmondellina) powersi, Oolina globosa, Nautiloculina oolithica, Kurnubia palastiniensis, Pseudomarssonella cf. maxima, Lenticulina sp. and two ostracod species: Hutsonia asiatica and Cytherella cf. umbilica. The survey of species covered in this research suggests that they indicate a predominantly euryhaline to polyhaline marine setting, possibly with a slightly brackish influence and deposited in a supratidal environment, suggesting a progressively shallowing environment on the inner shelf with intermittent shoal complexes.","PeriodicalId":49816,"journal":{"name":"Micropaleontology","volume":"1 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70445951","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
Ypresian Alveolina and calcareous nannofossils from the south Sabzevar area (Central Iran): biostratigraphic, taxonomic and paleobiogeographic implications 伊朗中部Sabzevar地区南部的伊朗牙槽藻和钙质纳米化石:生物地层、分类和古生物地理意义
IF 1.5 4区 地球科学
Micropaleontology Pub Date : 2021-01-01 DOI: 10.47894/mpal.67.1.04
M. Hadi, L. Consorti, M. Vahidinia, M. Parandavar, Marziyeh Zoraghi
{"title":"Ypresian Alveolina and calcareous nannofossils from the south Sabzevar area (Central Iran): biostratigraphic, taxonomic and paleobiogeographic implications","authors":"M. Hadi, L. Consorti, M. Vahidinia, M. Parandavar, Marziyeh Zoraghi","doi":"10.47894/mpal.67.1.04","DOIUrl":"https://doi.org/10.47894/mpal.67.1.04","url":null,"abstract":"The Eocene carbonates of the south Sabzevar region in central Iran hold a rich Alveolina assemblage.Nine species including A. globula, Alveolina sp. 1, Alveolina aff. globula, A. regularis, A. globosa, A. pasticillata, A. laxa, A. pisiformis and A. cf. decipiens are identified through detailed analysis in thin section. The biostratigraphy obtained points to the early Ypresian Shallow Benthic Zones SBZ6 and partly SBZ7, indicating the occurrence of a lower Eocene carbonate system. The Alveolina biostratigraphy is correlated to the calcareous nannofossil biostratigraphy, and is assignable to the middle part of the NP10 Zone and especially with the CNE2 biozones. The evolutionary trends of A. globula and its dispersal through thewestern and central Neo-Tethys Ocean during theYpresian is here considered in relation with the occurrence of Alveolina sp. 1.","PeriodicalId":49816,"journal":{"name":"Micropaleontology","volume":"1 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70444814","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
Gephyrocapsa kennettii sp. nov., a new calcareous nannofossil species from the Middle Pleistocene, Solomon Sea, western equatorial Pacific 赤道西太平洋所罗门海中更新世钙质纳米化石一新种Gephyrocapsa kennettii sp. nov.
IF 1.5 4区 地球科学
Micropaleontology Pub Date : 2021-01-01 DOI: 10.47894/mpal.67.1.01
C. Chuang, K. Wei, H. Mii, Hui-Ying Suk, L. Lo
{"title":"Gephyrocapsa kennettii sp. nov., a new calcareous nannofossil species from the Middle Pleistocene, Solomon Sea, western equatorial Pacific","authors":"C. Chuang, K. Wei, H. Mii, Hui-Ying Suk, L. Lo","doi":"10.47894/mpal.67.1.01","DOIUrl":"https://doi.org/10.47894/mpal.67.1.01","url":null,"abstract":"Detailed examinations of middle Pleistocene sediments of ODP Hole 1115B and CoreMD05-2925 in the Solomon Sea, southwest equatorial Pacific, reveal a distinctive new form of the calcareous nannofossil group of gephyrocapsid which has peculiar elongate kite-shaped slits on the distal shields of the coccolith. A new species,Gephyrocapsa kennettii sp. nov., is proposed and described in this study with SEM (scanning electron microscope) images. The coccolith of this new species is elliptical in shape, bearing 2 to 19 kite-shaped slits on the distal shield and a low-angle, raised arch-like bridge. The distal shield has fewer slits than G. protohuxleyi which has slits in between all elements. The bridge is orientated clockwise with am approximate 10 degree angle to the long axis when viewed distally. The average length of the distal shield is 3.26 plus or minus 0.22 (1 theta) mu m (n = 36), and, by definition, this new species belongs to the small Gephyrocapsa group. The chronologic range of this species is short, spanning only from 0.520–0.465 Ma. Its last occurrence datum is almost coevalwith that of Pseudoemiliania lacunosa at the bottom of Marine Isotope Stage 12. Morphologically, G. kennettii sp. nov. is intermediate between G. ericsonii and G. protohuxleyi and considered to be a transitional species originated by hybridization between them.","PeriodicalId":49816,"journal":{"name":"Micropaleontology","volume":"1 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70445079","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Stratigraphic development of a Late Oligocene Reef Complex under strong fluviatile influence in the Tertiary Piedmont Basin (Liguria, NWItaly) 强流体作用下第三系山前盆地晚渐新世礁杂岩的地层发育
IF 1.5 4区 地球科学
Micropaleontology Pub Date : 2021-01-01 DOI: 10.47894/mpal.67.4.01
A. Briguglio, G. Vannucci, Clarissa Bruzzone, M. Piazza
{"title":"Stratigraphic development of a Late Oligocene Reef Complex under strong fluviatile influence in the Tertiary Piedmont Basin (Liguria, NWItaly)","authors":"A. Briguglio, G. Vannucci, Clarissa Bruzzone, M. Piazza","doi":"10.47894/mpal.67.4.01","DOIUrl":"https://doi.org/10.47894/mpal.67.4.01","url":null,"abstract":"The modern-day decline of coral reefs due to bleaching events has been recognized as one of the major consequences of man-driven climate change. However, also eutrophication has been highlighted as an equally great danger for coral reefs and as such for biodiversity hotspots. In the latest years this phenomenon has moved to the forefront in the scientific community. Fossil reefs play a key role in studying the emergence, development and faunal/floral diversity of reef environments under eutrophic conditions. Their importance as valuable data sources for studying long-term changes of coral reef environments and their resilience cannot be disputed, especially since they may record the complete life cycle of a reef complex. In this study, nine sections nearby the town of Dego (Savona Province, NW Italy) are presented and discussed with regards to their lithostratigraphic and paleontological contents. Due to the extensive amount of data, the original morphology of a fringing reef, consisting of core, flank and fore reef, under strong fluviatile influence could be reconstructed. This study emphasizes the importance of the coralline red algae association in such biocarbonatic build-ups as major constituent and as substrate stabilizers. The sections record the original colonization event of the local basement by the builder community, the emergence of the coral reef and finally the suffocation by the fluviatile sediments. The variation of the red algae association reflects a deepening trend and is possibly correlated to enhanced fluvial input, which tends to deteriorate ecological conditions and functions as a major trigger for initial reef suffocation.","PeriodicalId":49816,"journal":{"name":"Micropaleontology","volume":"1 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70445379","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Elphidium tongaense (Cushman 1931), a quite old Recent foraminifer 汤加Elphidium tongaense (Cushman 1931),相当古老的近代有孔虫
IF 1.5 4区 地球科学
Micropaleontology Pub Date : 2021-01-01 DOI: 10.47894/mpal.67.4.05
S. Filipescu, Angela Miclea
{"title":"Elphidium tongaense (Cushman 1931), a quite old Recent foraminifer","authors":"S. Filipescu, Angela Miclea","doi":"10.47894/mpal.67.4.05","DOIUrl":"https://doi.org/10.47894/mpal.67.4.05","url":null,"abstract":"The late middleMiocene microfossil assemblages from the easternmost Pannonian Basin in Romania preserve numerous evolute and deformed specimens of Elphidium, which are assigned to the Recent species E. tongaense (Cushman 1931) originally described from the Pacific. Ourmaterial suggests that the origin of the species is back in the middle Miocene, when amarine connection between the Paratethys and the Indo-Pacific regions probably existed.","PeriodicalId":49816,"journal":{"name":"Micropaleontology","volume":"1 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70445645","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Roadian (earliest Guadalupian, middle Permian) radiolarians from the Guadalupe Mountains, West Texas, USA Part II: Spongy radiolarians (?Entactinaria and Spumellaria) 美国西德克萨斯州瓜达卢佩山脉的路迪亚纪(最早的瓜达卢佩纪,中二叠世)放射虫。第二部分:海绵状放射虫(?刺虫和刺虫)
IF 1.5 4区 地球科学
Micropaleontology Pub Date : 2021-01-01 DOI: 10.47894/mpal.67.6.01
G. Nestell, M. Nestell
{"title":"Roadian (earliest Guadalupian, middle Permian) radiolarians from the Guadalupe Mountains, West Texas, USA Part II: Spongy radiolarians (?Entactinaria and Spumellaria)","authors":"G. Nestell, M. Nestell","doi":"10.47894/mpal.67.6.01","DOIUrl":"https://doi.org/10.47894/mpal.67.6.01","url":null,"abstract":"Spongy radiolarians are described from strata of the Roadian Stage (Guadalupian, middle Permian) exposed in a small quarry (Quarry section) in the Guadalupe Mountains,West Texas. These radiolarians are assigned to the orders Entactinaria (conditionally) and Spumellaria. Two new families Hegleriidae and Glomispinidae are proposed. The genus Hegleria Nazarov and Ormiston and its two species, H. mammilla (Sheng andWang) and H. mammifera Nazarov and Ormiston are discussed. Based on an analysis of the distribution and preservation of the illustrated specimens of these two species in the literature, it is proposed that the species H. mammilla should be considered as nomen dubium. The genus Uberinterna Sashida and Tonishi and one species Copicyntra simulens Nazarov and Ormiston are revised. Five new genera, Texasospongites, Allenispongus, Cutoffella, Glomispina, and Orminazarella, and ten new species Texasospongites fazleevi, Allenispongus nobilis, Cutoffella perplexa, Glomispina mirifica, Uberinterna hearstae, U. ancestralis, Provisocyntra vancouveringi, Orminazarella nuda, Paracopicyntra bella, and Copiellintra variabilis are described.","PeriodicalId":49816,"journal":{"name":"Micropaleontology","volume":"1 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2021-01-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"70446145","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 7
Foraminifera in the glacial erratic rock Heiligenhafener Kieselgestein of northern Germany 德国北部Heiligenhafener-Kieselgestein冰川不稳定岩石中的有孔虫
IF 1.5 4区 地球科学
Micropaleontology Pub Date : 2020-09-01 DOI: 10.47894/mpal.66.5.03
M. Hesemann
{"title":"Foraminifera in the glacial erratic rock Heiligenhafener Kieselgestein of northern Germany","authors":"M. Hesemann","doi":"10.47894/mpal.66.5.03","DOIUrl":"https://doi.org/10.47894/mpal.66.5.03","url":null,"abstract":"In this study the foraminifera of the glacial erratic Heiligenhafener Kieselgestein (HKG) consisting of siliceous sandstones are documented for the first time. The glacial erratics in northern Germany were deposited during the Pleistocene. The age of the HKG sandstone is indicated as Eocene from 49.6 Ma to 47.8 Ma. The lower limit is given by the first occurrence of the planktonic foraminifera Pseudohastigerina micra (Cole 1927). The upper limit is derived from previous studies of the Eocene succession of Northern Germany based on benthic foraminiferal faunas. The HKG fauna indicates a boreal, fully marine environment characteristic for a water depth between 50 m and 80 m.","PeriodicalId":49816,"journal":{"name":"Micropaleontology","volume":" ","pages":""},"PeriodicalIF":1.5,"publicationDate":"2020-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"49421158","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Stratigraphic record of Eponides Montfort 1808 (benthic Foraminifera) through the Paleocene carbonates of the northern Neotethys margin 1808年Eponides Montfort(底栖有孔虫目)的地层记录,贯穿新特提斯北部边缘的古新世碳酸盐
IF 1.5 4区 地球科学
Micropaleontology Pub Date : 2020-09-01 DOI: 10.47894/mpal.66.5.01
L. Consorti, F. Schlagintweit, F. Koroglu, K. Rashidi
{"title":"Stratigraphic record of Eponides Montfort 1808 (benthic Foraminifera) through the Paleocene carbonates of the northern Neotethys margin","authors":"L. Consorti, F. Schlagintweit, F. Koroglu, K. Rashidi","doi":"10.47894/mpal.66.5.01","DOIUrl":"https://doi.org/10.47894/mpal.66.5.01","url":null,"abstract":"In the former northern Neotethys margin where Paleocene shallow-water limestone successions crop out (Austria, Turkey and Iran), morphotypes closely resembling Eponides have been recognized. These foraminifers are lamellar-perforated, with a trochospirally arranged set of trapezoidal chambers.We have tested their generic identification through a detailed architectural analysis of thin sections of carbonate rocks in which Eponides-like specimens have abundantly been recovered. This study shows the occurrence of bipartitor, arched septa and a pseudoumbilicus formed by the fusion of ventral ends of chambers. These features allow us to identify the specimens as Eponides, although the specific attribution has not been attempted. The evolutionary pattern displayed by the Late Cretaceous and Cenozoic Eponides and phylogenetically-related allies is briefly discussed.","PeriodicalId":49816,"journal":{"name":"Micropaleontology","volume":" ","pages":""},"PeriodicalIF":1.5,"publicationDate":"2020-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"43478548","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
New names for the species Nodosaria catenulata Karavaeva and Nestell 2007 and Nodosaria costata Karavaeva and Nestell 2007 (Foraminifera) catenulata Nodosaria Karavaeva和Nestell 2007和costata Nodosaria Karavaeva和Nestell 2007的新名称(有孔虫目)
IF 1.5 4区 地球科学
Micropaleontology Pub Date : 2020-09-01 DOI: 10.47894/mpal.66.5.07
Nelly I. Karavaeva, G. Nestell
{"title":"New names for the species Nodosaria catenulata Karavaeva and Nestell 2007 and Nodosaria costata Karavaeva and Nestell 2007 (Foraminifera)","authors":"Nelly I. Karavaeva, G. Nestell","doi":"10.47894/mpal.66.5.07","DOIUrl":"https://doi.org/10.47894/mpal.66.5.07","url":null,"abstract":"The names of the two species Nodosaria catenulata Karavaeva and Nestell 2007 and Nodosaria costata Karavaeva and Nestell 2007 described from Permian strata of the Omolon Massif, northeastern Siberia, Russia (Karavaeva and Nestell 2007) are preoccupied and are junior homonyms of previously described species.","PeriodicalId":49816,"journal":{"name":"Micropaleontology","volume":"1 1","pages":""},"PeriodicalIF":1.5,"publicationDate":"2020-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"41991149","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
Loftusia persica Brady, a Maastrichtian larger benthic foraminifera and not an Eocene Lazarus taxon Loftusia persica Brady,马斯特里赫特阶大型底栖有孔虫,不是始新世Lazarus分类单元
IF 1.5 4区 地球科学
Micropaleontology Pub Date : 2020-09-01 DOI: 10.47894/mpal.66.5.04
F. Schlagintweit, Hossein Ghanbarloo, A. Safari, H. Vaziri-Moghaddam
{"title":"Loftusia persica Brady, a Maastrichtian larger benthic foraminifera and not an Eocene Lazarus taxon","authors":"F. Schlagintweit, Hossein Ghanbarloo, A. Safari, H. Vaziri-Moghaddam","doi":"10.47894/mpal.66.5.04","DOIUrl":"https://doi.org/10.47894/mpal.66.5.04","url":null,"abstract":"","PeriodicalId":49816,"journal":{"name":"Micropaleontology","volume":" ","pages":""},"PeriodicalIF":1.5,"publicationDate":"2020-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46921054","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":4,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 0
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