Pub Date : 2023-12-28DOI: 10.1007/s41513-023-00226-6
Ignacio Díaz-Martínez, Paolo Citton, D. Castanera
{"title":"¿Qué nos dicen sus huellas? Muchas preguntas y algunas respuestas sobre la vida de los dinosaurios no avianos","authors":"Ignacio Díaz-Martínez, Paolo Citton, D. Castanera","doi":"10.1007/s41513-023-00226-6","DOIUrl":"https://doi.org/10.1007/s41513-023-00226-6","url":null,"abstract":"","PeriodicalId":54799,"journal":{"name":"Journal of Iberian Geology","volume":"41 8","pages":""},"PeriodicalIF":1.3,"publicationDate":"2023-12-28","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139149500","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}
Pub Date : 2023-12-12DOI: 10.1007/s41513-023-00225-7
Chaouki Khalfi, R. Ahmadi, Eric Mercier
{"title":"New insights based on the reinterpretation of the geophysical data for the suggestion of a model of the Bouhlel anticline in the Southern Tunisian Atlas front","authors":"Chaouki Khalfi, R. Ahmadi, Eric Mercier","doi":"10.1007/s41513-023-00225-7","DOIUrl":"https://doi.org/10.1007/s41513-023-00225-7","url":null,"abstract":"","PeriodicalId":54799,"journal":{"name":"Journal of Iberian Geology","volume":"66 7","pages":""},"PeriodicalIF":1.3,"publicationDate":"2023-12-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139008267","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}
Pub Date : 2023-11-22DOI: 10.1007/s41513-023-00218-6
A. R. Rosa, P. Cachapuz, T. D. dos Santos, I. Pereira, Á. R. Solá, D. R. Carvalho, J. Romão, P. Vaquero
{"title":"Tales from xenoliths: the link between the Papôa Volcanic Breccia and the Berlengas Archipelago (West Portugal)—geodynamic implications","authors":"A. R. Rosa, P. Cachapuz, T. D. dos Santos, I. Pereira, Á. R. Solá, D. R. Carvalho, J. Romão, P. Vaquero","doi":"10.1007/s41513-023-00218-6","DOIUrl":"https://doi.org/10.1007/s41513-023-00218-6","url":null,"abstract":"","PeriodicalId":54799,"journal":{"name":"Journal of Iberian Geology","volume":"12 1","pages":"275 - 364"},"PeriodicalIF":1.3,"publicationDate":"2023-11-22","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139246570","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}
Pub Date : 2023-11-21DOI: 10.1007/s41513-023-00224-8
Mehrdad Balouch, Majid Nemati, M. Bagheripour, Ahmad Rashidi
{"title":"A probabilistic seismic hazard analysis in SE Iran; case study: Kerman province","authors":"Mehrdad Balouch, Majid Nemati, M. Bagheripour, Ahmad Rashidi","doi":"10.1007/s41513-023-00224-8","DOIUrl":"https://doi.org/10.1007/s41513-023-00224-8","url":null,"abstract":"","PeriodicalId":54799,"journal":{"name":"Journal of Iberian Geology","volume":"165 3","pages":"257 - 274"},"PeriodicalIF":1.3,"publicationDate":"2023-11-21","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"139252977","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}
Pub Date : 2023-11-10DOI: 10.1007/s41513-023-00221-x
Abdelhamid M. Salman, Mohammad A. Sarhan, Mohamed M. Elhossainy
{"title":"Estratigrafía de secuencias e investigación petrofísica de sedimentos fluviales: Un estudio de caso Arenisca de Nubia, yacimiento de Ras Budran, Golfo de Suez, Egipto","authors":"Abdelhamid M. Salman, Mohammad A. Sarhan, Mohamed M. Elhossainy","doi":"10.1007/s41513-023-00221-x","DOIUrl":"https://doi.org/10.1007/s41513-023-00221-x","url":null,"abstract":"","PeriodicalId":54799,"journal":{"name":"Journal of Iberian Geology","volume":"106 2","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-11-10","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135136253","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}
Pub Date : 2023-11-09DOI: 10.1007/s41513-023-00223-9
E. Medrano-Aguado, J. Parrilla-Bel, J. I. Canudo
{"title":"Correction: Palaeobiodiversity of Sauropoda in the Blesa Formation (Lower Cretaceous) at northeast Spain","authors":"E. Medrano-Aguado, J. Parrilla-Bel, J. I. Canudo","doi":"10.1007/s41513-023-00223-9","DOIUrl":"https://doi.org/10.1007/s41513-023-00223-9","url":null,"abstract":"","PeriodicalId":54799,"journal":{"name":"Journal of Iberian Geology","volume":" 5","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-11-09","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135242576","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}
Pub Date : 2023-10-25DOI: 10.1007/s41513-023-00220-y
E. Puértolas-Pascual, M. Aurell, D. D. Bermúdez-Rochas, J. I. Canudo, A. E. Fernandes, A. Galobart, M. Moreno-Azanza, A. Pérez-García, D. Castanera
Abstract The Ribota site (Ágreda, Soria, Spain) is a new locality in the Matute Formation (Tithonian–Berriasian) composed of several carbonate layers, outstandingly rich in macrovertebrate remains. Fossils show an unusual replacement of the original bioapatite by quartz, and are found as positive reliefs protruding from lacustrine limestone beds. This type of conservation has allowed the identification of around one hundred vertebrate bone accumulations in an outcrop of more than 10 hectares. Osteichthyans (articulated partial skeletons, cranial material, and isolated postcranial bones and scales), crocodylomorphs (disarticulated cranial material, isolated teeth, vertebrae and osteoderms), turtles (partial carapaces and plastra, but also isolated plates) and pterosaurs (cranial and appendicular elements) have been identified. Around 80 specimens have been collected and a preliminary study of part of the collection (35 specimens) has allowed the identification of at least 5 different taxa: Halecomorphi indet., Neoginglymodi indet., Goniopholididae indet., Testudinata indet., and Pterodactyloidea indet. This new site represents one of the few sites from this time interval preserved in a fully lacustrine environment, so these vertebrate assemblages are unique and composed of different animals that presumably lived around and within the lake. They are dominated by aquatic and amphibian vertebrates and was formed by attrition in this lacustrine environment, possibly far from the lake shoreline. These macrovertebrate assemblages provide new data about the diversity in the faunal ecosystems from the Jurassic/Cretaceous transition of the Iberian Basin Rift System.
Ribota遗址(Ágreda, Soria, Spain)是Matute组(Tithonian-Berriasian)中的一个新地点，由几个碳酸盐层组成，非常丰富的大型脊椎动物遗骸。化石显示石英代替了原始的生物磷灰石，并在湖相灰岩床中被发现为凸出的正面浮雕。这种类型的保护使得在超过10公顷的露头中发现了大约100个脊椎动物的骨头。已经鉴定出了骨鱼目动物(关节部分骨骼、颅骨材料和分离的颅后骨骼和鳞片)、鳄鱼形动物(分离的颅骨材料、分离的牙齿、椎骨和骨皮)、海龟(部分甲壳和骨质，但也有分离的板)和翼龙(颅骨和阑尾部分)。已经收集了大约80个标本，对部分标本(35个标本)的初步研究已经确定了至少5个不同的分类群:Halecomorphi indet。我不知道。Goniopholididae indet;， Testudinata indet。和翼手亚目。这个新遗址是这段时间内保存在完全湖泊环境中的少数遗址之一，所以这些脊椎动物的组合是独特的，由可能生活在湖周围和湖中的不同动物组成。它们以水生和两栖脊椎动物为主，是在远离湖岸线的湖泊环境中由磨蚀作用形成的。这些大型脊椎动物组合为研究伊比利亚盆地裂谷系侏罗纪/白垩纪过渡时期动物生态系统的多样性提供了新的数据。
{"title":"A new vertebrate assemblage from the matute formation of the Cameros Basin (Ágreda, Spain): implications for the diversity during the jurassic/cretaceous boundary","authors":"E. Puértolas-Pascual, M. Aurell, D. D. Bermúdez-Rochas, J. I. Canudo, A. E. Fernandes, A. Galobart, M. Moreno-Azanza, A. Pérez-García, D. Castanera","doi":"10.1007/s41513-023-00220-y","DOIUrl":"https://doi.org/10.1007/s41513-023-00220-y","url":null,"abstract":"Abstract The Ribota site (Ágreda, Soria, Spain) is a new locality in the Matute Formation (Tithonian–Berriasian) composed of several carbonate layers, outstandingly rich in macrovertebrate remains. Fossils show an unusual replacement of the original bioapatite by quartz, and are found as positive reliefs protruding from lacustrine limestone beds. This type of conservation has allowed the identification of around one hundred vertebrate bone accumulations in an outcrop of more than 10 hectares. Osteichthyans (articulated partial skeletons, cranial material, and isolated postcranial bones and scales), crocodylomorphs (disarticulated cranial material, isolated teeth, vertebrae and osteoderms), turtles (partial carapaces and plastra, but also isolated plates) and pterosaurs (cranial and appendicular elements) have been identified. Around 80 specimens have been collected and a preliminary study of part of the collection (35 specimens) has allowed the identification of at least 5 different taxa: Halecomorphi indet., Neoginglymodi indet., Goniopholididae indet., Testudinata indet., and Pterodactyloidea indet. This new site represents one of the few sites from this time interval preserved in a fully lacustrine environment, so these vertebrate assemblages are unique and composed of different animals that presumably lived around and within the lake. They are dominated by aquatic and amphibian vertebrates and was formed by attrition in this lacustrine environment, possibly far from the lake shoreline. These macrovertebrate assemblages provide new data about the diversity in the faunal ecosystems from the Jurassic/Cretaceous transition of the Iberian Basin Rift System.","PeriodicalId":54799,"journal":{"name":"Journal of Iberian Geology","volume":"24 13","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-10-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135113640","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}
Pub Date : 2023-10-19DOI: 10.1007/s41513-023-00222-w
Eduardo Mayoral, Cayetano Herrero, Emilio Herrero, Javier Martín‑Chivelet, Félix Pérez‑Lorente
{"title":"Correction: A new enigmatic lacustrine trackway in the upper Miocene of the Sierra de las Cabras (Jumilla, Murcia, Spain)","authors":"Eduardo Mayoral, Cayetano Herrero, Emilio Herrero, Javier Martín‑Chivelet, Félix Pérez‑Lorente","doi":"10.1007/s41513-023-00222-w","DOIUrl":"https://doi.org/10.1007/s41513-023-00222-w","url":null,"abstract":"","PeriodicalId":54799,"journal":{"name":"Journal of Iberian Geology","volume":"29 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-10-19","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135730188","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}
Pub Date : 2023-10-15DOI: 10.1007/s41513-023-00219-5
E. Medrano-Aguado, J. Parrilla-Bel, J. I. Canudo
Abstract The Blesa Formation is one of the richest formations of the Barremian of the Iberian Peninsula in terms of vertebrate biodiversity. In the La Cantalera-1 site more than 32 vertebrate taxa have been identified, but the only sauropod remains are three isolated teeth related to Euhelopodidae. In this paper, all the sauropod material studied so far in this formation is reviewed and new remains are described. The material comes from different sites in all three depositional sequences of the Blesa Formation. A new tooth, a fragmented cervical vertebra and a caudal vertebra are described in the La Cantalera-1 site and assigned tentatively to Euhelopodidae. One left tibia, one left ischium and one caudal vertebra have been recovered in different fossils sites in the Lower, Middle and Upper Blesa sequences respectively. These new sauropod remains are assigned to Titanosauriformes, the most common group of dinosaurs in the Barremian of the Iberian Peninsula. The isolated character of the fossils precludes more precise taxonomic attributions.
{"title":"Paleobiodiversidad de Sauropoda en la Formación Blesa (Cretácico Inferior) en el noreste de España","authors":"E. Medrano-Aguado, J. Parrilla-Bel, J. I. Canudo","doi":"10.1007/s41513-023-00219-5","DOIUrl":"https://doi.org/10.1007/s41513-023-00219-5","url":null,"abstract":"Abstract The Blesa Formation is one of the richest formations of the Barremian of the Iberian Peninsula in terms of vertebrate biodiversity. In the La Cantalera-1 site more than 32 vertebrate taxa have been identified, but the only sauropod remains are three isolated teeth related to Euhelopodidae. In this paper, all the sauropod material studied so far in this formation is reviewed and new remains are described. The material comes from different sites in all three depositional sequences of the Blesa Formation. A new tooth, a fragmented cervical vertebra and a caudal vertebra are described in the La Cantalera-1 site and assigned tentatively to Euhelopodidae. One left tibia, one left ischium and one caudal vertebra have been recovered in different fossils sites in the Lower, Middle and Upper Blesa sequences respectively. These new sauropod remains are assigned to Titanosauriformes, the most common group of dinosaurs in the Barremian of the Iberian Peninsula. The isolated character of the fossils precludes more precise taxonomic attributions.","PeriodicalId":54799,"journal":{"name":"Journal of Iberian Geology","volume":"1 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-10-15","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"136185256","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}
Pub Date : 2023-09-12DOI: 10.1007/s41513-023-00217-7
F. Torcida Fernández-Baldor, P. Huerta, E. Puértolas-Pascual, J. I. Canudo
Abstract In this work, a dentary, and several teeth from the Valdepalazuelos-Tenadas del Carrascal site (Burgos, Spain) are studied. Geologically,this site is situatedat the base of the Rupelo Formation (Cuenca de Cameros), of Tithonian–Berriasian age. This formation has been interpreted as lacustrine-palustrine deposits with low gradient margins and with periodic changes in the water level. MDS-VPCR,851 is a fragment of the rostral symphyseal zone of a right dentary, a robust bone with a rostral ridge on its lingual surface, large diameter foramina on the lingual surface, a wide Meckelian canal extending from the rostroventral margin, semicircular symphysis arranged rostrolingually, and with two alveoli preserving two erupting teetheach. Although the functional teeth have not been preserved, each alveolus could contain one active tooth and at least two replacement teeth. Eight maxillary and mandibular teeth are described, with a spatulate crown, a rough enamel surface, a D-shaped croos-section, and a very marked cingulum. The dentary and teeth from this site have evident differences with those of other taxa and specimens described in the Kimmeridgian-Berriasian of the Iberian Peninsula. Its greatest similarities are with Camarasaurus , but in the specimens from Valdepalazuelos there are characters that seem to be unique and differ from that taxon. Consequently. the specimens described here are identified as belonging to a basal macronarian, close to Camarasaurus . This work points to the existence of two macronarian sauropods in the Tithonian–Berriasian transit of the Cameros Basin, and increases the diversity of the Iberian record of that time period.
在这项工作中，研究了来自Valdepalazuelos-Tenadas del Carrascal遗址(Burgos, Spain)的一颗牙齿和几颗牙齿。从地质学上讲，该遗址位于Tithonian-Berriasian时代的Rupelo地层(Cuenca de Cameros)的底部。该地层被解释为具有低梯度边缘和水位周期性变化的湖滩沉积。MDS-VPCR,851是右侧牙槽骨的吻侧联合区片段，骨强壮，舌面有吻侧脊，舌面有大直径的椎间孔，从牙腹侧缘延伸出宽的Meckelian管，半圆形联合向舌侧排列，两个牙槽各保留两颗出牙。虽然没有保留功能牙，但每个牙槽可包含一颗活动牙和至少两颗替代牙。描述了八颗上颌和下颌牙齿，具有匙形冠，粗糙的牙釉质表面，d形十字形截面和非常明显的扣带。该遗址的齿状和牙齿与伊比利亚半岛的Kimmeridgian-Berriasian中描述的其他分类群和标本有明显差异。它与圆顶龙最相似，但在瓦尔德帕拉苏埃洛斯的标本中，有一些特征似乎是独特的，与那个分类单元不同。因此。这里描述的标本被鉴定为属于基隆龙，接近圆顶龙。这项工作指出，在喀麦隆盆地的提索尼亚-贝里亚过渡时期存在两种大型蜥脚类动物，并增加了伊比利亚时期记录的多样性。
{"title":"Nuevos dientes de un macronario basal (Sauropoda) del Tránsito Jurásico-Cretácico de España","authors":"F. Torcida Fernández-Baldor, P. Huerta, E. Puértolas-Pascual, J. I. Canudo","doi":"10.1007/s41513-023-00217-7","DOIUrl":"https://doi.org/10.1007/s41513-023-00217-7","url":null,"abstract":"Abstract In this work, a dentary, and several teeth from the Valdepalazuelos-Tenadas del Carrascal site (Burgos, Spain) are studied. Geologically,this site is situatedat the base of the Rupelo Formation (Cuenca de Cameros), of Tithonian–Berriasian age. This formation has been interpreted as lacustrine-palustrine deposits with low gradient margins and with periodic changes in the water level. MDS-VPCR,851 is a fragment of the rostral symphyseal zone of a right dentary, a robust bone with a rostral ridge on its lingual surface, large diameter foramina on the lingual surface, a wide Meckelian canal extending from the rostroventral margin, semicircular symphysis arranged rostrolingually, and with two alveoli preserving two erupting teetheach. Although the functional teeth have not been preserved, each alveolus could contain one active tooth and at least two replacement teeth. Eight maxillary and mandibular teeth are described, with a spatulate crown, a rough enamel surface, a D-shaped croos-section, and a very marked cingulum. The dentary and teeth from this site have evident differences with those of other taxa and specimens described in the Kimmeridgian-Berriasian of the Iberian Peninsula. Its greatest similarities are with Camarasaurus , but in the specimens from Valdepalazuelos there are characters that seem to be unique and differ from that taxon. Consequently. the specimens described here are identified as belonging to a basal macronarian, close to Camarasaurus . This work points to the existence of two macronarian sauropods in the Tithonian–Berriasian transit of the Cameros Basin, and increases the diversity of the Iberian record of that time period.","PeriodicalId":54799,"journal":{"name":"Journal of Iberian Geology","volume":"20 1","pages":"0"},"PeriodicalIF":0.0,"publicationDate":"2023-09-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"135880733","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}
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