Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.1127/nos/2019/0525 |
Tephrochronology and chronostratigraphy of the Miocene Chilcatay and Pisco formations (East Pisco Basin, Peru) | |
Bosio, Giulia1; Malinverno, Elisa1; Villa, Igor Maria1,2; Di Celma, Claudio3; Gariboldi, Karen4; Gioncada, Anna4; Barberini, Valentina1; Urbina, Mario5; Bianucci, Giovanni4 | |
通讯作者 | Bosio, Giulia |
来源期刊 | NEWSLETTERS ON STRATIGRAPHY
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ISSN | 0078-0421 |
出版年 | 2020 |
卷号 | 53期号:2页码:213-247 |
英文摘要 | Strata of Chilcatay and Pisco formations exposed in the Ica Desert (East Pisco Basin, southern Peru) preserve one of the most complete and rich records of Miocene marine vertebrates of the world. Despite its exceptional importance, the chronostratigraphy of these fossil-bearing deposits has been only sporadically studied in the literature until recently. This work presents a detailed reconstruction of the chronostratigraphic framework, achieved by mapping and logging of seven sections of the Miocene Chilcatay and Pisco formations along the western side of the Ica River. The Chilcatay Formation consists of two allomembers, namely Ct1 and Ct2, bounded at the base by unconformities CE0.1 and CE0.2, respectively. Similarly, the immediately overlying Pisco Formation is divided into allomembers P0, P1, and P2, bounded at the base by unconformities PE0.0, PE0.1 and PE0.2, respectively. The new Ar-39-Ar-4(0) results presented here, combined with ages of previous work, provide precise constraints on the age of several stratigraphically referenced volcanic ash layers intercalated in the studied fossil-bearing succession, placing its vertebrate fossil fauna within a refined temporal framework and laying the solid ground for its detailed regional and global comparison. The ages of the allomembers, and thus their associated faunas, can be reliably estimated by the combination of Ar-39-Ar-40 dating on tephra layers with diatom biostratigraphy. In the study area, the two methods are mutually consistent and constrain the deposition of the Chilcatay Formation between 19.2 and 18.0 Ma, that of P1 between 9.5 and 8.6 Ma, and that of P2 between 8.4 and 6.7 Ma. In the absence of direct dating of the P0 allomember, which lacks both preserved tephra suitable for Ar-39-Ar-40 dating and microfossils, its age can be constrained to the temporal gap between the youngest age available from the underlying Chilcatay strata (18.0 Ma) and the oldest age available from the overlying P1 strata (9.5 Ma). |
英文关键词 | tephrochronology tephrostratigraphy Ar-39-Ar-40 dating biostratigraphy Miocene Pisco Basin |
类型 | Article |
语种 | 英语 |
国家 | Italy ; Peru |
收录类别 | SCI-E |
WOS记录号 | WOS:000541129400004 |
WOS关键词 | FOSSIL MARINE VERTEBRATES ; AR-40/AR-39 GEOCHRONOLOGY ; CERRO COLORADO ; FORE-ARC ; NEOGENE ; STRATIGRAPHY ; RECORD ; PALEONTOLOGY ; PRESERVATION ; ODONTOCETI |
WOS类目 | Geology |
WOS研究方向 | Geology |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/319714 |
作者单位 | 1.Univ Milano Bicocca, Dipartimento Sci Ambiente & Terra, I-20126 Milan, Italy; 2.Univ Milano Bicocca, Ctr Univ Dataz & Archeometria, I-20126 Milan, Italy; 3.Univ Camerino, Scuola Sci & Tecnol, I-62032 Camerino, Italy; 4.Univ Pisa, Dipartimento Sci Terra, I-56126 Pisa, Italy; 5.Univ Nacl Mayor San Marcos, Museo Hist Nat, UNMSM, Dept Paleontol Vertebrados, Lima 1, Peru |
推荐引用方式 GB/T 7714 | Bosio, Giulia,Malinverno, Elisa,Villa, Igor Maria,et al. Tephrochronology and chronostratigraphy of the Miocene Chilcatay and Pisco formations (East Pisco Basin, Peru)[J],2020,53(2):213-247. |
APA | Bosio, Giulia.,Malinverno, Elisa.,Villa, Igor Maria.,Di Celma, Claudio.,Gariboldi, Karen.,...&Bianucci, Giovanni.(2020).Tephrochronology and chronostratigraphy of the Miocene Chilcatay and Pisco formations (East Pisco Basin, Peru).NEWSLETTERS ON STRATIGRAPHY,53(2),213-247. |
MLA | Bosio, Giulia,et al."Tephrochronology and chronostratigraphy of the Miocene Chilcatay and Pisco formations (East Pisco Basin, Peru)".NEWSLETTERS ON STRATIGRAPHY 53.2(2020):213-247. |
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