{"title":"斯洛文尼亚西北部卡拉万克山脉Belca剖面“Raibl Beds”(卡尼阶,三叠纪晚期)的介形虫","authors":"M. Forel, T. Kolar-Jurkovšek, B. Jurkovšek","doi":"10.5252/geodiversitas2020v42a21","DOIUrl":null,"url":null,"abstract":"ABSTRACT The taxonomy of marine ostracod assemblages from Belca section in the Karavanke Mountains, northwestern Slovenia, is discussed, adding to the scientific understanding of marine ostracods during the Carnian stage, Late Triassic. In Belca, the ostracod assemblages include 39 species, among which two are newly described: Dicerobairdia buseri Forel, n. sp. and Pontocypris? karavankensis Forel, n. sp. The recovery of abundant juvenile and adult specimens facilitated the illustration and discussion of the ontogenetic series of several typically Triassic species including Renngartenella sanctaecrucis Kris-tan-Tollmann in Kristan-Tollmann & Hamedani, 1973, Leviella bogschi Kozur, 1972 and Leviella veghae Kozur, 1972. The occurrence of sexual dimorphism is furthermore confirmed for Renngartenella sanctaecrucis. Ostracods in Belca record a major shift from low diversity and high dominance assemblages at the base of the section to higher diversity and lower dominance with diversification of stable open-marine taxa in the upper part. This pattern might illustrate low salinity levels related to high land-derived input at the base of the section and a return to relatively normal marine salinity in the intermediate sublittoral zone in the upper portion of Belca section.","PeriodicalId":55111,"journal":{"name":"Geodiversitas","volume":"42 1","pages":"377 - 407"},"PeriodicalIF":1.5000,"publicationDate":"2020-09-01","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"7","resultStr":"{\"title\":\"Ostracods from the ‘Raibl Beds’ (Carnian, Late Triassic) of Belca section in Karavanke Mountains, northwestern Slovenia\",\"authors\":\"M. Forel, T. Kolar-Jurkovšek, B. Jurkovšek\",\"doi\":\"10.5252/geodiversitas2020v42a21\",\"DOIUrl\":null,\"url\":null,\"abstract\":\"ABSTRACT The taxonomy of marine ostracod assemblages from Belca section in the Karavanke Mountains, northwestern Slovenia, is discussed, adding to the scientific understanding of marine ostracods during the Carnian stage, Late Triassic. In Belca, the ostracod assemblages include 39 species, among which two are newly described: Dicerobairdia buseri Forel, n. sp. and Pontocypris? karavankensis Forel, n. sp. The recovery of abundant juvenile and adult specimens facilitated the illustration and discussion of the ontogenetic series of several typically Triassic species including Renngartenella sanctaecrucis Kris-tan-Tollmann in Kristan-Tollmann & Hamedani, 1973, Leviella bogschi Kozur, 1972 and Leviella veghae Kozur, 1972. The occurrence of sexual dimorphism is furthermore confirmed for Renngartenella sanctaecrucis. Ostracods in Belca record a major shift from low diversity and high dominance assemblages at the base of the section to higher diversity and lower dominance with diversification of stable open-marine taxa in the upper part. This pattern might illustrate low salinity levels related to high land-derived input at the base of the section and a return to relatively normal marine salinity in the intermediate sublittoral zone in the upper portion of Belca section.\",\"PeriodicalId\":55111,\"journal\":{\"name\":\"Geodiversitas\",\"volume\":\"42 1\",\"pages\":\"377 - 407\"},\"PeriodicalIF\":1.5000,\"publicationDate\":\"2020-09-01\",\"publicationTypes\":\"Journal Article\",\"fieldsOfStudy\":null,\"isOpenAccess\":false,\"openAccessPdf\":\"\",\"citationCount\":\"7\",\"resultStr\":null,\"platform\":\"Semanticscholar\",\"paperid\":null,\"PeriodicalName\":\"Geodiversitas\",\"FirstCategoryId\":\"89\",\"ListUrlMain\":\"https://doi.org/10.5252/geodiversitas2020v42a21\",\"RegionNum\":3,\"RegionCategory\":\"地球科学\",\"ArticlePicture\":[],\"TitleCN\":null,\"AbstractTextCN\":null,\"PMCID\":null,\"EPubDate\":\"\",\"PubModel\":\"\",\"JCR\":\"Q2\",\"JCRName\":\"PALEONTOLOGY\",\"Score\":null,\"Total\":0}","platform":"Semanticscholar","paperid":null,"PeriodicalName":"Geodiversitas","FirstCategoryId":"89","ListUrlMain":"https://doi.org/10.5252/geodiversitas2020v42a21","RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"PALEONTOLOGY","Score":null,"Total":0}
Ostracods from the ‘Raibl Beds’ (Carnian, Late Triassic) of Belca section in Karavanke Mountains, northwestern Slovenia
ABSTRACT The taxonomy of marine ostracod assemblages from Belca section in the Karavanke Mountains, northwestern Slovenia, is discussed, adding to the scientific understanding of marine ostracods during the Carnian stage, Late Triassic. In Belca, the ostracod assemblages include 39 species, among which two are newly described: Dicerobairdia buseri Forel, n. sp. and Pontocypris? karavankensis Forel, n. sp. The recovery of abundant juvenile and adult specimens facilitated the illustration and discussion of the ontogenetic series of several typically Triassic species including Renngartenella sanctaecrucis Kris-tan-Tollmann in Kristan-Tollmann & Hamedani, 1973, Leviella bogschi Kozur, 1972 and Leviella veghae Kozur, 1972. The occurrence of sexual dimorphism is furthermore confirmed for Renngartenella sanctaecrucis. Ostracods in Belca record a major shift from low diversity and high dominance assemblages at the base of the section to higher diversity and lower dominance with diversification of stable open-marine taxa in the upper part. This pattern might illustrate low salinity levels related to high land-derived input at the base of the section and a return to relatively normal marine salinity in the intermediate sublittoral zone in the upper portion of Belca section.
期刊介绍:
Geodiversitas is a fully electronic journal, with a continuous publication stream, devoted to varied aspects of Earth Sciences. It publishes original results particularly on systematics, phylogeny, paleobiodiversity and paleoenvironment.
Thematic issues may also be published under the responsibility of a guest editor.