Pub Date : 2022-06-05DOI: 10.3140/bull.geosci.1851
T. Weiner, H. Weinerová, M. Mergl, J. Kalvoda, R. Gregorová
of the Moravosilesian Basin in Czech Republic (Fig. 1) has rarely been documented. Brachiopods have only briefly been discussed or mentioned (e.g. Rak et al. 2012) and trilobites were depicted and described by Chlupáč (1961, 1966) and Rak et al. (2012). The Palaeozoic sequences of the Moravosilesian Basin were exposed to extensive erosion. However, eroded material has been partly preserved in younger sedimentary units, mainly Variscan and Carpathian flysch and molasse sediments. The composition of basal and marginal coarse clastics deposited during the early Badenian transgression in the Carpathian Foredeep reflects the varied provenance of the source material (Brzobohatý & Cicha 1993). Krystek (1974) has recognized 14 types of rock clasts of these clastics between Brno and Prostějov. Dark grey limestone clasts have generally been considered Devonian (e.g. Šob 1940, Krystek 1974), but they have not been studied in detail. In this study, we share information obtained from a limestone boulder, showing that it is of late Tournaisian age, thereby enabling us to contribute to the discussion regarding the provenance of Badenian basal clastics. Brachiopod and trilobite fauna of this boulder proves valuable with respect to our knowledge of the Palaeozoic macrofauna of the Moravosilesian Basin.
{"title":"Carboniferous limestone boulder from the Badenian clastics (Carpathian Foredeep, Czech Republic): A useful data source on the Palaeozoic of the Moravosilesian Basin","authors":"T. Weiner, H. Weinerová, M. Mergl, J. Kalvoda, R. Gregorová","doi":"10.3140/bull.geosci.1851","DOIUrl":"https://doi.org/10.3140/bull.geosci.1851","url":null,"abstract":"of the Moravosilesian Basin in Czech Republic (Fig. 1) has rarely been documented. Brachiopods have only briefly been discussed or mentioned (e.g. Rak et al. 2012) and trilobites were depicted and described by Chlupáč (1961, 1966) and Rak et al. (2012). The Palaeozoic sequences of the Moravosilesian Basin were exposed to extensive erosion. However, eroded material has been partly preserved in younger sedimentary units, mainly Variscan and Carpathian flysch and molasse sediments. The composition of basal and marginal coarse clastics deposited during the early Badenian transgression in the Carpathian Foredeep reflects the varied provenance of the source material (Brzobohatý & Cicha 1993). Krystek (1974) has recognized 14 types of rock clasts of these clastics between Brno and Prostějov. Dark grey limestone clasts have generally been considered Devonian (e.g. Šob 1940, Krystek 1974), but they have not been studied in detail. In this study, we share information obtained from a limestone boulder, showing that it is of late Tournaisian age, thereby enabling us to contribute to the discussion regarding the provenance of Badenian basal clastics. Brachiopod and trilobite fauna of this boulder proves valuable with respect to our knowledge of the Palaeozoic macrofauna of the Moravosilesian Basin.","PeriodicalId":9332,"journal":{"name":"Bulletin of Geosciences","volume":" ","pages":""},"PeriodicalIF":1.9,"publicationDate":"2022-06-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42731480","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-06-05DOI: 10.3140/bull.geosci.1841
AleksAndr, s., BAkAev, Ilja Kogan
occur in the continental upper Permian successions of European Russia. Due to their abundance and character istic morphology, they have been used as index fossils for biostratigraphic zonation schemes in order to define substagelevel assemblage zones and even the socalled Toyemia superassemblage zone, slightly exceeding the duration of a stage (Esin & Mashin 1996, Minikh & Minikh 2009). The onset of this superassemblage, cha r acterized by a high degree of endemism, coincides with the disappearance of several generalist fish forms as well as shifts in tetrapod and aquatic invertebrate communities, and has been interpreted in the context of major palaeoenvironmental changes on a regional scale (Bakaev et al. 2017). Toyemia was originally described as a member of Gonatodidae Gardiner, 1967, although similarities with the scanilepiform Evenkia Berg, 1941 have equally been pointed out (Minikh & Minikh 1990). Toyemia is reconstructed as a mediumsized predator of freshwater habitats (Minikh & Minikh 2009, Romano et al. 2016). For a better understanding of the palaeobiology and interrelationships of this both ecologically and strati graphically significant taxon, we are conducting a com prehensive morphological study based on new and rediscovered, previously undescribed material. In this contribution, we present new morphological and histo l ogical data on the squamation of Toyemia and the evenkiids Evenkia and Oshia Sytchevskaya, 1999, and discuss their possible phylogenetic implications.
{"title":"Squamation of the Permian actinopterygian Toyemia Minich, 1990: evenkiid (Scanilepiformes) affinities and implications for the origin of polypteroid scales","authors":"AleksAndr, s., BAkAev, Ilja Kogan","doi":"10.3140/bull.geosci.1841","DOIUrl":"https://doi.org/10.3140/bull.geosci.1841","url":null,"abstract":"occur in the continental upper Permian successions of European Russia. Due to their abundance and character istic morphology, they have been used as index fossils for biostratigraphic zonation schemes in order to define substagelevel assemblage zones and even the socalled Toyemia superassemblage zone, slightly exceeding the duration of a stage (Esin & Mashin 1996, Minikh & Minikh 2009). The onset of this superassemblage, cha r acterized by a high degree of endemism, coincides with the disappearance of several generalist fish forms as well as shifts in tetrapod and aquatic invertebrate communities, and has been interpreted in the context of major palaeoenvironmental changes on a regional scale (Bakaev et al. 2017). Toyemia was originally described as a member of Gonatodidae Gardiner, 1967, although similarities with the scanilepiform Evenkia Berg, 1941 have equally been pointed out (Minikh & Minikh 1990). Toyemia is reconstructed as a mediumsized predator of freshwater habitats (Minikh & Minikh 2009, Romano et al. 2016). For a better understanding of the palaeobiology and interrelationships of this both ecologically and strati graphically significant taxon, we are conducting a com prehensive morphological study based on new and rediscovered, previously undescribed material. In this contribution, we present new morphological and histo l ogical data on the squamation of Toyemia and the evenkiids Evenkia and Oshia Sytchevskaya, 1999, and discuss their possible phylogenetic implications.","PeriodicalId":9332,"journal":{"name":"Bulletin of Geosciences","volume":" ","pages":""},"PeriodicalIF":1.9,"publicationDate":"2022-06-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45029450","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-06-05DOI: 10.3140/bull.geosci.1848
Mona Mandor, O. Vinn, M. E. Hedeny, aHMed el, SabbagH, Abdelaal Abdelaal, MoHaMed raSHwan
(e.g. Gosselin & Sewell 2013) from the Permian (Sanfilippo et al. 2017) to the present day (e.g. Rouse & Pleijel 2001). Most tube-building polychaete worms are benthic and sedentary suspension feeders (e.g. Díaz-Castañeda & Reish 2009). Serpulid-like calcareous tubes displayed a rapid diversification throughout the Jurassic and Cretaceous until the Holocene (Jäger 1983, 2004, 2012, 2014; Ippolitov 2007a, b, 2010; Sklenář et al. 2013; Ippolitov et al. 2014; Kočí & Ledvák 2014; Kočí et al. 2017). They secrete and inhabit a permanent calcareous tube that can be attached to both biogenic and inorganic hard substrates. They are most commonly found as post-mortem encrusters (e.g. Garberoglio & Lazo 2011, Sklenář et al. 2013, El-Sabbagh & El Hedeny 2016, El-Sabbagh et al. 2016, Veselská et al. 2021) but may also be colonizers of living hosts (in vivo; e.g. El Hedeny et al. 2021). Hard substrates in the modern oceans are often heavily encrusted by polychaetes. They are common in all marine settings, ranging from the intertidal down to hadal depths (e.g. Hill 2013, Ippolitov et al. 2014). In addition, they were important encrusting organisms in the geological past (e.g. El-Sabbagh & El Hedeny 2016, El-Sabbagh et al. 2016). Hence, the study of ancient representatives could provide information on palaeoecology and palaeoenvironment. Sediments of the lower‒middle Miocene succession exposed in the Cairo-Suez District yield a significant polychaete assemblage, which, together with bivalves (oysters, pectinids and others), gastropods and echinoids, constitute the characteristic fossil assemblage in that area. Other common fossils include corals and bryozoans. So far, little attention has been paid to fossil calcareous tubedwelling encrusting polychaetes in Egypt (e.g. El-Sabbagh & El Hedeny 2016, El-Sabbagh et al. 2016). Therefore, this
(例如Gosselin & Sewell 2013)从二叠纪(Sanfilippo et al. 2017)到现在(例如Rouse & Pleijel 2001)。大多数建管多毛类蠕虫是底栖和静止的悬浮食性蠕虫(例如Díaz-Castañeda & Reish 2009)。蛇形钙质管在整个侏罗纪和白垩纪到全新世期间表现出快速的多样化(Jäger 1983, 2004, 2012, 2014;伊波利托夫，2007a, b, 2010;Sklenář et al. 2013;Ippolitov et al. 2014;Kočí & Ledvák 2014;Kočí et al. 2017)。它们分泌并栖息在一个永久的钙质管中，这个管可以附着在生物和无机的硬基质上。它们最常被发现为死后结块(例如Garberoglio & Lazo 2011, Sklenář et al. 2013, El- sabbagh & El Hedeny 2016, El- sabbagh et al. 2016, veselsk et al. 2021)，但也可能是活体宿主的殖民者(在体内;例如El Hedeny et al. 2021)。现代海洋中的坚硬底物经常被多毛体包裹着。它们在所有海洋环境中都很常见，从潮间带到潮深(例如Hill 2013, Ippolitov et al. 2014)。此外，它们在地质历史上是重要的覆壳生物(例如El- sabbagh & El Hedeny 2016, El- sabbagh et al. 2016)。因此，对古代表物的研究可以提供有关古生态和古环境的信息。在开罗-苏伊士地区暴露的中新世中下序列沉积物中，发现了大量的多毛类组合，与双壳类(牡蛎、果胶类等)、腹足类和棘足类一起构成了该地区的典型化石组合。其他常见的化石包括珊瑚和苔藓虫。到目前为止，很少有人关注埃及的化石钙质套管覆壳多毛体(例如El- sabbagh & El Hedeny 2016, El- sabbagh et al. 2016)。因此,该
{"title":"Calcareous tube-dwelling encrusting polychaetes from a lower-middle Miocene sedimentary succession, Cairo-Suez District, Egypt","authors":"Mona Mandor, O. Vinn, M. E. Hedeny, aHMed el, SabbagH, Abdelaal Abdelaal, MoHaMed raSHwan","doi":"10.3140/bull.geosci.1848","DOIUrl":"https://doi.org/10.3140/bull.geosci.1848","url":null,"abstract":"(e.g. Gosselin & Sewell 2013) from the Permian (Sanfilippo et al. 2017) to the present day (e.g. Rouse & Pleijel 2001). Most tube-building polychaete worms are benthic and sedentary suspension feeders (e.g. Díaz-Castañeda & Reish 2009). Serpulid-like calcareous tubes displayed a rapid diversification throughout the Jurassic and Cretaceous until the Holocene (Jäger 1983, 2004, 2012, 2014; Ippolitov 2007a, b, 2010; Sklenář et al. 2013; Ippolitov et al. 2014; Kočí & Ledvák 2014; Kočí et al. 2017). They secrete and inhabit a permanent calcareous tube that can be attached to both biogenic and inorganic hard substrates. They are most commonly found as post-mortem encrusters (e.g. Garberoglio & Lazo 2011, Sklenář et al. 2013, El-Sabbagh & El Hedeny 2016, El-Sabbagh et al. 2016, Veselská et al. 2021) but may also be colonizers of living hosts (in vivo; e.g. El Hedeny et al. 2021). Hard substrates in the modern oceans are often heavily encrusted by polychaetes. They are common in all marine settings, ranging from the intertidal down to hadal depths (e.g. Hill 2013, Ippolitov et al. 2014). In addition, they were important encrusting organisms in the geological past (e.g. El-Sabbagh & El Hedeny 2016, El-Sabbagh et al. 2016). Hence, the study of ancient representatives could provide information on palaeoecology and palaeoenvironment. Sediments of the lower‒middle Miocene succession exposed in the Cairo-Suez District yield a significant polychaete assemblage, which, together with bivalves (oysters, pectinids and others), gastropods and echinoids, constitute the characteristic fossil assemblage in that area. Other common fossils include corals and bryozoans. So far, little attention has been paid to fossil calcareous tubedwelling encrusting polychaetes in Egypt (e.g. El-Sabbagh & El Hedeny 2016, El-Sabbagh et al. 2016). Therefore, this","PeriodicalId":9332,"journal":{"name":"Bulletin of Geosciences","volume":" ","pages":""},"PeriodicalIF":1.9,"publicationDate":"2022-06-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"44527222","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-06-05DOI: 10.3140/bull.geosci.1845
A. Ivanov
(Mississippian) of European part of Russia are common, rather diverse and have been quite well studied (Romanowsky 1864, Trautschold 1874, Khabakov 1941, Obruchev 1977, Ivanov & Ginter 1996, Lebedev 1996, and others). The chondrichthyan assemblages from the Bashkirian–Moscovian (Pennsylvanian) of this territory have also been described in many publications (e.g. Traut schold 1879, Khabakov 1939, Obruchev 1951, Le bedev 2001, and others). However, chondrichthyan fishes are poorly known from the Kasimovian–Gzhelian of this area. The remains of diverse chondrichthyans were re cently found in the Kasimovian–Gzhelian deposits of the Moscow, Samara and Volgograd regions, and in the Bashkirian–Moscovian of the Republic of Bashkortostan. The remains are represented by isolated teeth and scales of various chondrichthyan groups and mostly belong to known taxa. However, three new taxa presented by teeth occurred in these stratigraphical intervals and regions, and are described in this paper.
{"title":"New late Carboniferous chondrichthyans from the European Russia","authors":"A. Ivanov","doi":"10.3140/bull.geosci.1845","DOIUrl":"https://doi.org/10.3140/bull.geosci.1845","url":null,"abstract":"(Mississippian) of European part of Russia are common, rather diverse and have been quite well studied (Romanowsky 1864, Trautschold 1874, Khabakov 1941, Obruchev 1977, Ivanov & Ginter 1996, Lebedev 1996, and others). The chondrichthyan assemblages from the Bashkirian–Moscovian (Pennsylvanian) of this territory have also been described in many publications (e.g. Traut schold 1879, Khabakov 1939, Obruchev 1951, Le bedev 2001, and others). However, chondrichthyan fishes are poorly known from the Kasimovian–Gzhelian of this area. The remains of diverse chondrichthyans were re cently found in the Kasimovian–Gzhelian deposits of the Moscow, Samara and Volgograd regions, and in the Bashkirian–Moscovian of the Republic of Bashkortostan. The remains are represented by isolated teeth and scales of various chondrichthyan groups and mostly belong to known taxa. However, three new taxa presented by teeth occurred in these stratigraphical intervals and regions, and are described in this paper.","PeriodicalId":9332,"journal":{"name":"Bulletin of Geosciences","volume":" ","pages":""},"PeriodicalIF":1.9,"publicationDate":"2022-06-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42979106","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-06-05DOI: 10.3140/bull.geosci.1856
Joaquín Albesa, J. M. Lopez, Vicente, D., Crespo
such as those of Vallés-Penedés, Ebro, Calatayud-Daroca, Teruel, Duero and Tajo, as well as smaller ones such as Cabriel, Fortuna, Guadix-Baza and Granada (Agustí 2018). Continental sediments of Aragonian age (end of the early Miocene to middle Miocene; mammal biozones MN4 to MN7/8) are represented in many of these basins (Agustí 2018). While mammal associations have been studied extensively in several palaeontological sites, the malacological record is comparatively poor documented. The few studies carried out on the malacological assemblages recorded in sediments today attributed to an Aragonian age are to some extent outdated (Vilanova y Piera 1859; Royo Gómez 1922, 1926, 1928; Jodot 1959). Also, many of sites and faunas documented in these works could not be precisely located. The available references accurately located and dated correspond to sites attributed to the middle Aragonian of the Tajo Basin (Truc 1977) and the upper Aragonian of the Duero Basin (González Delgado et al. 1986, Civis et al. 1989). The references from the early Aragonian are practically inexistent and correspond to isolated cites or recent multidisciplinary studies in the Ribesalbes-Alcora Basin (Peñalver et al. 2016, ÁlvarezParra et al. 2021). In line with the above, the available data on the mala cological content of the sediments of the Ribesalbes-Alcora Basin (Fig. 1A) are mostly old and very scarce. The first one corresponds to Vilanova y Piera (1859) who studied the materials in the “Balsa de Fanzaraˮ (the classical name for the Cenozoic sediments of the basin) and the nearby area of Alcalá. He cited the generic presence of “lymneasˮ, “planorbis” and “helicesˮ (Vilanova y Piera 1859: p. 44), and more specifically a single specimen of Planorbis rotundatus Brongniart, 1810 from the “Balsa de Fanzara”, which is shown on a plate alongside with four species belonging to the Alcalá area. Royo Gómez (1922) included a brief reference to the sediments of the studied area correcting the determination of Planorbis rotundatus to
例如瓦尔萨-佩内德-卡、埃布罗、卡拉塔尤德-达罗卡、特鲁埃尔、杜埃罗和塔霍，以及较小的卡布里埃尔、福尔图纳、瓜迪克斯-巴扎和格拉纳达(Agustí 2018)。阿拉贡时代(早中新世末至中新世中期)的陆相沉积物;这些盆地中有许多哺乳动物生物带(MN4至MN7/8) (Agustí 2018)。虽然哺乳动物的关联已经在几个古生物遗址进行了广泛的研究，但线虫学的记录相对较少。目前对阿拉贡时代沉积物中记录的虫藻学组合进行的少数研究在某种程度上是过时的(Vilanova y Piera 1859;罗约Gómez 1922、1926、1928;Jodot 1959)。此外，这些作品中记录的许多地点和动物无法精确定位。现有的准确定位和年代的参考资料对应于Tajo盆地的中阿拉贡期(Truc 1977)和Duero盆地的上阿拉贡期(González Delgado et al. 1986, Civis et al. 1989)。来自阿拉贡期早期的文献几乎不存在，与Ribesalbes-Alcora盆地的孤立城市或最近的多学科研究相对应(Peñalver et al. 2016， ÁlvarezParra et al. 2021)。综上所述，关于Ribesalbes-Alcora盆地沉积物的mala生态学含量的现有数据(图1A)大多是古老的，非常稀少。第一个对应于Vilanova y Piera(1859)，他研究了“Balsa de Fanzara”(盆地新生代沉积物的经典名称)和alcal附近地区的物质。他引用了“lyneas”，“planorbis”和“helices”的普遍存在(Vilanova y Piera 1859:第44页)，更具体地说，1810年来自“Balsa de Fanzara”的planorbis rotundatus Brongniart的单一标本，与属于alcal地区的四个物种一起显示在一个盘子上。Royo Gómez(1922)包含了对研究区域沉积物的简要参考，纠正了对圆形planoris的测定
{"title":"Filling the gap in knowledge of early Miocene continental molluscs of southwest Europe: gastropods from Ribesalbes-Alcora Basin (Spain)","authors":"Joaquín Albesa, J. M. Lopez, Vicente, D., Crespo","doi":"10.3140/bull.geosci.1856","DOIUrl":"https://doi.org/10.3140/bull.geosci.1856","url":null,"abstract":"such as those of Vallés-Penedés, Ebro, Calatayud-Daroca, Teruel, Duero and Tajo, as well as smaller ones such as Cabriel, Fortuna, Guadix-Baza and Granada (Agustí 2018). Continental sediments of Aragonian age (end of the early Miocene to middle Miocene; mammal biozones MN4 to MN7/8) are represented in many of these basins (Agustí 2018). While mammal associations have been studied extensively in several palaeontological sites, the malacological record is comparatively poor documented. The few studies carried out on the malacological assemblages recorded in sediments today attributed to an Aragonian age are to some extent outdated (Vilanova y Piera 1859; Royo Gómez 1922, 1926, 1928; Jodot 1959). Also, many of sites and faunas documented in these works could not be precisely located. The available references accurately located and dated correspond to sites attributed to the middle Aragonian of the Tajo Basin (Truc 1977) and the upper Aragonian of the Duero Basin (González Delgado et al. 1986, Civis et al. 1989). The references from the early Aragonian are practically inexistent and correspond to isolated cites or recent multidisciplinary studies in the Ribesalbes-Alcora Basin (Peñalver et al. 2016, ÁlvarezParra et al. 2021). In line with the above, the available data on the mala cological content of the sediments of the Ribesalbes-Alcora Basin (Fig. 1A) are mostly old and very scarce. The first one corresponds to Vilanova y Piera (1859) who studied the materials in the “Balsa de Fanzaraˮ (the classical name for the Cenozoic sediments of the basin) and the nearby area of Alcalá. He cited the generic presence of “lymneasˮ, “planorbis” and “helicesˮ (Vilanova y Piera 1859: p. 44), and more specifically a single specimen of Planorbis rotundatus Brongniart, 1810 from the “Balsa de Fanzara”, which is shown on a plate alongside with four species belonging to the Alcalá area. Royo Gómez (1922) included a brief reference to the sediments of the studied area correcting the determination of Planorbis rotundatus to","PeriodicalId":9332,"journal":{"name":"Bulletin of Geosciences","volume":" ","pages":""},"PeriodicalIF":1.9,"publicationDate":"2022-06-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42974436","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-06-05DOI: 10.3140/bull.geosci.1842
I. Hradská, S. Opluštil, P. Selden, J. Dunlop
1949) are representatives of an extinct group of somewhat spider-like arachnids known from the upper Silurian (Přídolí) to the lower Permian (Sakmarian); see Dunlop & Rößler (2013) for a summary of their localities and stratigraphic distribution. Trigonotarbids are usually resolved in the arachnid clade Pantetrapulmonata (e.g. Garwood & Dunlop 2014) as the sister-group of Tetrapulmonata, i.e. the orders Araneae (spiders), Amblypygi (whip spiders), Thelyphonida (whip scorp ions) and Schizomida (schizomids). Trigonotarbids also share characters with the order Ricinulei (hooded tick spiders), such as an opisthosoma with longitudinally divided tergites, a locking mechanism between the prosoma and opisthosoma and a small claw at the tip of the pedipalp (e.g. Dunlop et al. 2009). Trigonotarbid fossils are characterised by a segmented opisthosoma with eight or nine dorsally visible tergites, most of which are, as noted above, divided longitudinally into median and lateral plates. These animals evidently had mouthparts modified for biting in the form of ‘clasp-knife’ chelicerae (Garwood & Dunlop 2010; Haug 2018, 2020) and were presumably predators in Palaeozoic terrestrial ecosystems. Around a hundred species of trigonotarbid have been described in the literature, of which 70 are currently considered valid (Dunlop et al. 2020). Fourteen of them are known from the Czech Republic, and historical descriptions can be found in Stur (1877), Kušta (1883, 1884), Frič (1901, 1904), Petrunkevitch (1953) and Přibyl (1958). More recent summaries and species descriptions can be found in Opluštil (1985, 1986), with a revision of three genera by Dunlop (1995) and the description of a further new species by Hradská & Dunlop (2013). Here, we describe a new genus and species of an unusually gracile trigonotarbid from the Pennsylvanian (early Moscovian) Radnice Member of the Pilsen Basin.
{"title":"A new species of trigonotarbid arachnid from the Pilsen Basin of the Czech Republic","authors":"I. Hradská, S. Opluštil, P. Selden, J. Dunlop","doi":"10.3140/bull.geosci.1842","DOIUrl":"https://doi.org/10.3140/bull.geosci.1842","url":null,"abstract":"1949) are representatives of an extinct group of somewhat spider-like arachnids known from the upper Silurian (Přídolí) to the lower Permian (Sakmarian); see Dunlop & Rößler (2013) for a summary of their localities and stratigraphic distribution. Trigonotarbids are usually resolved in the arachnid clade Pantetrapulmonata (e.g. Garwood & Dunlop 2014) as the sister-group of Tetrapulmonata, i.e. the orders Araneae (spiders), Amblypygi (whip spiders), Thelyphonida (whip scorp ions) and Schizomida (schizomids). Trigonotarbids also share characters with the order Ricinulei (hooded tick spiders), such as an opisthosoma with longitudinally divided tergites, a locking mechanism between the prosoma and opisthosoma and a small claw at the tip of the pedipalp (e.g. Dunlop et al. 2009). Trigonotarbid fossils are characterised by a segmented opisthosoma with eight or nine dorsally visible tergites, most of which are, as noted above, divided longitudinally into median and lateral plates. These animals evidently had mouthparts modified for biting in the form of ‘clasp-knife’ chelicerae (Garwood & Dunlop 2010; Haug 2018, 2020) and were presumably predators in Palaeozoic terrestrial ecosystems. Around a hundred species of trigonotarbid have been described in the literature, of which 70 are currently considered valid (Dunlop et al. 2020). Fourteen of them are known from the Czech Republic, and historical descriptions can be found in Stur (1877), Kušta (1883, 1884), Frič (1901, 1904), Petrunkevitch (1953) and Přibyl (1958). More recent summaries and species descriptions can be found in Opluštil (1985, 1986), with a revision of three genera by Dunlop (1995) and the description of a further new species by Hradská & Dunlop (2013). Here, we describe a new genus and species of an unusually gracile trigonotarbid from the Pennsylvanian (early Moscovian) Radnice Member of the Pilsen Basin.","PeriodicalId":9332,"journal":{"name":"Bulletin of Geosciences","volume":" ","pages":""},"PeriodicalIF":1.9,"publicationDate":"2022-06-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46978610","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-06-05DOI: 10.3140/bull.geosci.1846
D. Knaust, R. Mikuláš, M. Mángano, Rangel Cerceau Netto, L. Buatois
reconstructions (e.g. Pemberton 1992, Pemberton et al. 2001, Buatois & Mángano 2011, Knaust & Bromley 2012) and for detecting evolutionary trends (e.g. Mángano & Buatois 2016a, b). Increased interest in ichnology resulted in the description and erection of numerous ichnotaxa that allowed for their recurrent recognition and communication. However, after the compilation of the second edition of the Trace Fossils volume in the Treatise of Invertebrate Paleontology (Häntzschel 1975), the number of valid invertebrate ichnogenera has multiplied (Knaust 2012, Buatois et al. 2017). Many ichnotaxa are based on weak grounds, either due to in appropriate characteristics chosen as ichnotaxobases, poor preservation, single specimens, or simply overlooked synonymy. Accordingly, comprehensive ichnotaxonomic reciews are necessary for the efficient and robust applic a tion of ichnologic evidence. This contribution provides a taxonomic assessment of the ichnospecies Curvolithus gregarius Fritsch, 1908 from the Upper Ordovician of Czechia (see Mikuláš 1992, for previous evaluations of this ichnofauna), based on a reinvestigation of the type material and newly col lected specimens. In a general review of the ichnogenus Curvolithus, Buatois et al. (1998) excluded the ichno species C. gregarius from that ichnogenus due to the morphological discrepancy with the diagnostic features of Curvolithus. These authors also noted similarities of the type material of C. gregarius with other scratched trace fossils supposedly produced by arthropods, such as Tam bia and Monomorphichnus. However, no formal ichno taxo n omic decision was made at that time, and the ichno taxon omic status of this ichno species was left indeterminate. Here, we formally include C. gregarius in Tambia Müller, 1969 as T. gregaria comb. nov. In addition, we briefly revise other ichnotaxa described by Fritsch (1908) that are related to T. gregaria. This study is part of an overall examination of historical tracefossil collections and ichnotaxonomic reevaluation of the collection of Fritsch (1908) at the National Museum in Prague, Czechia.
重建(例如Pemberton 1992, Pemberton et al. 2001, Buatois & Mángano 2011, Knaust & Bromley 2012)以及检测进化趋势(例如Mángano & Buatois 2016a, b)。对技术的兴趣增加导致了许多鱼分类群的描述和建立，使它们能够反复识别和交流。然而，在《无脊椎动物古生物学专著》(Häntzschel 1975)中“微量化石”卷第二版的编纂之后，有效的无脊椎动物技术属的数量成倍增加(Knaust 2012, Buatois et al. 2017)。许多鱼分类群是建立在薄弱的基础上的，要么是由于选择了不适当的特征作为鱼分类基，要么是保存不良，要么是标本单一，要么是简单地忽视了同义。因此，全面的技术分类知识库是技术证据有效、可靠应用的必要条件。本文对捷克上奥陶统的Curvolithus gregarius Fritsch, 1908进行了分类评估(见Mikuláš 1992，对该鱼科动物的先前评价)，基于对模式材料和新收集的标本的重新调查。Buatois et al.(1998)在对Curvolithus鱼属的综述中，由于与Curvolithus的诊断特征在形态上的差异，将该鱼属中的ichno - species C. gregarius排除在外。这些作者还注意到C. gregarius的类型材料与其他被认为是节肢动物(如Tam bia和Monomorphichnus)产生的划痕痕迹化石的相似性。然而，当时没有正式的鱼类分类组决定，该物种的鱼类分类组地位仍然不确定。在这里，我们正式将C. gregarius in Tambia mller, 1969作为T. gregaria comb。11 .此外，对Fritsch(1908)所描述的与T. gregaria有亲缘关系的其他ichnotaxa进行了简要的修正。这项研究是对捷克布拉格国家博物馆的历史化石收藏和弗里奇(1908)收藏的技术分类重新评估的整体检查的一部分。
{"title":"The ichnospecies Tambia gregaria (Fritsch, 1908) comb. nov. from the Upper Ordovician of Czechia","authors":"D. Knaust, R. Mikuláš, M. Mángano, Rangel Cerceau Netto, L. Buatois","doi":"10.3140/bull.geosci.1846","DOIUrl":"https://doi.org/10.3140/bull.geosci.1846","url":null,"abstract":"reconstructions (e.g. Pemberton 1992, Pemberton et al. 2001, Buatois & Mángano 2011, Knaust & Bromley 2012) and for detecting evolutionary trends (e.g. Mángano & Buatois 2016a, b). Increased interest in ichnology resulted in the description and erection of numerous ichnotaxa that allowed for their recurrent recognition and communication. However, after the compilation of the second edition of the Trace Fossils volume in the Treatise of Invertebrate Paleontology (Häntzschel 1975), the number of valid invertebrate ichnogenera has multiplied (Knaust 2012, Buatois et al. 2017). Many ichnotaxa are based on weak grounds, either due to in appropriate characteristics chosen as ichnotaxobases, poor preservation, single specimens, or simply overlooked synonymy. Accordingly, comprehensive ichnotaxonomic reciews are necessary for the efficient and robust applic a tion of ichnologic evidence. This contribution provides a taxonomic assessment of the ichnospecies Curvolithus gregarius Fritsch, 1908 from the Upper Ordovician of Czechia (see Mikuláš 1992, for previous evaluations of this ichnofauna), based on a reinvestigation of the type material and newly col lected specimens. In a general review of the ichnogenus Curvolithus, Buatois et al. (1998) excluded the ichno species C. gregarius from that ichnogenus due to the morphological discrepancy with the diagnostic features of Curvolithus. These authors also noted similarities of the type material of C. gregarius with other scratched trace fossils supposedly produced by arthropods, such as Tam bia and Monomorphichnus. However, no formal ichno taxo n omic decision was made at that time, and the ichno taxon omic status of this ichno species was left indeterminate. Here, we formally include C. gregarius in Tambia Müller, 1969 as T. gregaria comb. nov. In addition, we briefly revise other ichnotaxa described by Fritsch (1908) that are related to T. gregaria. This study is part of an overall examination of historical tracefossil collections and ichnotaxonomic reevaluation of the collection of Fritsch (1908) at the National Museum in Prague, Czechia.","PeriodicalId":9332,"journal":{"name":"Bulletin of Geosciences","volume":" ","pages":""},"PeriodicalIF":1.9,"publicationDate":"2022-06-05","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"42257751","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-01-23DOI: 10.3140/bull.geosci.1800
S. Zorina
{"title":"Black shales contamination and depositional paleoenvironment during the Early Aptian OAE 1a in the Eastern Russian Platform","authors":"S. Zorina","doi":"10.3140/bull.geosci.1800","DOIUrl":"https://doi.org/10.3140/bull.geosci.1800","url":null,"abstract":"","PeriodicalId":9332,"journal":{"name":"Bulletin of Geosciences","volume":" ","pages":""},"PeriodicalIF":1.9,"publicationDate":"2022-01-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"45975158","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-01-23DOI: 10.3140/bull.geosci.1834
R. Feist, G. Klapper
{"title":"Phacopid trilobites in post-Taghanic Givetian through Frasnian cephalopod limestones, Montagne Noire (France) and related areas (Thuringia, Morocco)","authors":"R. Feist, G. Klapper","doi":"10.3140/bull.geosci.1834","DOIUrl":"https://doi.org/10.3140/bull.geosci.1834","url":null,"abstract":"","PeriodicalId":9332,"journal":{"name":"Bulletin of Geosciences","volume":" ","pages":""},"PeriodicalIF":1.9,"publicationDate":"2022-01-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"48038483","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
Pub Date : 2022-01-23DOI: 10.3140/bull.geosci.1818
M. Hörnig, C. Haug, P. Müller, J. T. Haug
{"title":"Not quite social - possible cases of gregarious behaviour of immatures of various lineages of Insecta in 100-million-year-old amber","authors":"M. Hörnig, C. Haug, P. Müller, J. T. Haug","doi":"10.3140/bull.geosci.1818","DOIUrl":"https://doi.org/10.3140/bull.geosci.1818","url":null,"abstract":"","PeriodicalId":9332,"journal":{"name":"Bulletin of Geosciences","volume":" ","pages":""},"PeriodicalIF":1.9,"publicationDate":"2022-01-23","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"46280118","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":3,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
京公网安备 11010802042870号
京ICP备2023020795号-1
扫码关注我们
求助内容：
应助结果提醒方式：