The “Lochkovian-Pragian Event” re-assessed: New data from the low latitude shelf of peri-Gondwana

IF 2.6 2区 地球科学 Q2 GEOGRAPHY, PHYSICAL
Carlo Corradini , Maria G. Corriga , Monica Pondrelli , Amalia Spina , Thomas J. Suttner
{"title":"The “Lochkovian-Pragian Event” re-assessed: New data from the low latitude shelf of peri-Gondwana","authors":"Carlo Corradini ,&nbsp;Maria G. Corriga ,&nbsp;Monica Pondrelli ,&nbsp;Amalia Spina ,&nbsp;Thomas J. Suttner","doi":"10.1016/j.palaeo.2024.112580","DOIUrl":null,"url":null,"abstract":"<div><div>In the late Lochkovian a regression is documented in several areas of the world, followed by a transgression in the early Pragian. Connected with the eustatic variation, a minor extinction event occurred (“Lochkovian-Pragian Event”), affecting several fossil groups, a strong reduction of carbonate production and sedimentary facies changes. The Carnic Alps are a key area for studying this event, because Lower Devonian rocks are widely exposed, representing diverse sedimentary environments from shallow water to relatively deep shelf. Fourteen sections were measured along the Carnic Alps across the Lochkovian-Pragian boundary. In the shallower part of the basin, both the Polinik and the Seekopf formations span the boundary, but evident erosional surfaces are observable in the field at the Lochkovian-Pragian boundary. Above the unconformity, at places the so-called megaclast horizon is present in the Seekopf Formation. In intermediate settings the Rauchkofel Fm. is unconfomably followed by the Kellerwand Fm., and different parts of the upper Lochkovian and lower Pragian are missing in the various sections. In the deeper parts of the basin the transition from the La Valute Fm. to the Findenig Fm. is slightly diachronous from the latest Lochkovian to the earliest Pragian; however, conodonts and tentaculitids are rare in the marly boundary beds, preventing a precise chronostratigraphic calibration of these levels. At places, evidence of subaerial exposure at the formational boundary is documented. In general, the hiatus seems to be larger in the western part of the Carnic Alps, in correspondence with the shallower parts of the succession, suggesting a sea level drop in the late Lochkovian, followed by a transgression in the Pragian. Data from the Carnic Alps are compared with those of other regions of North Gondwana to demonstrate that the sea-level variation at the Lochkovian-Pragian boundary are of global importance</div></div>","PeriodicalId":19928,"journal":{"name":"Palaeogeography, Palaeoclimatology, Palaeoecology","volume":"656 ","pages":"Article 112580"},"PeriodicalIF":2.6000,"publicationDate":"2024-11-02","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Palaeogeography, Palaeoclimatology, Palaeoecology","FirstCategoryId":"89","ListUrlMain":"https://www.sciencedirect.com/science/article/pii/S0031018224005698","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"GEOGRAPHY, PHYSICAL","Score":null,"Total":0}
引用次数: 0

Abstract

In the late Lochkovian a regression is documented in several areas of the world, followed by a transgression in the early Pragian. Connected with the eustatic variation, a minor extinction event occurred (“Lochkovian-Pragian Event”), affecting several fossil groups, a strong reduction of carbonate production and sedimentary facies changes. The Carnic Alps are a key area for studying this event, because Lower Devonian rocks are widely exposed, representing diverse sedimentary environments from shallow water to relatively deep shelf. Fourteen sections were measured along the Carnic Alps across the Lochkovian-Pragian boundary. In the shallower part of the basin, both the Polinik and the Seekopf formations span the boundary, but evident erosional surfaces are observable in the field at the Lochkovian-Pragian boundary. Above the unconformity, at places the so-called megaclast horizon is present in the Seekopf Formation. In intermediate settings the Rauchkofel Fm. is unconfomably followed by the Kellerwand Fm., and different parts of the upper Lochkovian and lower Pragian are missing in the various sections. In the deeper parts of the basin the transition from the La Valute Fm. to the Findenig Fm. is slightly diachronous from the latest Lochkovian to the earliest Pragian; however, conodonts and tentaculitids are rare in the marly boundary beds, preventing a precise chronostratigraphic calibration of these levels. At places, evidence of subaerial exposure at the formational boundary is documented. In general, the hiatus seems to be larger in the western part of the Carnic Alps, in correspondence with the shallower parts of the succession, suggesting a sea level drop in the late Lochkovian, followed by a transgression in the Pragian. Data from the Carnic Alps are compared with those of other regions of North Gondwana to demonstrate that the sea-level variation at the Lochkovian-Pragian boundary are of global importance

Abstract Image

重新评估 "洛克维安-普拉格安事件":来自近冈瓦纳低纬度大陆架的新数据
据记载,在洛克维期晚期,世界多个地区出现了退缩,随后在普拉格期早期出现了横断。与震旦纪变迁相关联,发生了一次小规模的生物大灭绝事件("洛克维期-普拉格期事件"),影响了多个化石群,碳酸盐生成量大幅减少,沉积面貌也发生了变化。卡尼阿尔卑斯山是研究这一事件的关键地区,因为下泥盆统岩石广泛出露,代表了从浅水到相对较深的陆架的各种沉积环境。我们沿卡尼阿尔卑斯山脉测量了 14 个横跨洛克维期-普拉格期边界的断面。在盆地较浅的地方,波利尼克地层和西科普夫地层都跨越了边界,但在洛可可维-普拉西边界的实地观察中,可以看到明显的侵蚀面。在不整合层之上,Seekopf 地层中有些地方出现了所谓的巨岩层。在中间地带,Rauchkofel 地层之后是 Kellerwand 地层,在不同的地段,上 Lochkovian 和下 Pragian 的不同部分缺失。在盆地较深的地方,从最晚的洛克维期到最早的普拉格期,从 La Valute Fm. 到 Findenig Fm. 的过渡略显不同步;然而,在泥灰质边界床中,锥齿类和触角类非常罕见,因此无法对这些层位进行精确的年代地层校准。在一些地方,有形成边界次生暴露的证据。总体而言,卡尼阿尔卑斯山西部的断裂似乎较大,与演替的较浅部分相对应,这表明海平面在洛克维期晚期下降,随后在普拉格期发生了横断。将卡尼阿尔卑斯山的数据与北冈瓦纳其他地区的数据进行了比较,以证明洛克维期-普拉格期边界的海平面变化具有全球重要性。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
求助全文
约1分钟内获得全文 求助全文
来源期刊
CiteScore
5.90
自引率
10.00%
发文量
398
审稿时长
3.8 months
期刊介绍: Palaeogeography, Palaeoclimatology, Palaeoecology is an international medium for the publication of high quality and multidisciplinary, original studies and comprehensive reviews in the field of palaeo-environmental geology. The journal aims at bringing together data with global implications from research in the many different disciplines involved in palaeo-environmental investigations. By cutting across the boundaries of established sciences, it provides an interdisciplinary forum where issues of general interest can be discussed.
×
引用
GB/T 7714-2015
复制
MLA
复制
APA
复制
导出至
BibTeX EndNote RefMan NoteFirst NoteExpress
×
提示
您的信息不完整,为了账户安全,请先补充。
现在去补充
×
提示
您因"违规操作"
具体请查看互助需知
我知道了
×
提示
确定
请完成安全验证×
copy
已复制链接
快去分享给好友吧!
我知道了
右上角分享
点击右上角分享
0
联系我们:info@booksci.cn Book学术提供免费学术资源搜索服务,方便国内外学者检索中英文文献。致力于提供最便捷和优质的服务体验。 Copyright © 2023 布克学术 All rights reserved.
京ICP备2023020795号-1
ghs 京公网安备 11010802042870号
Book学术文献互助
Book学术文献互助群
群 号:481959085
Book学术官方微信