Knowledge Resource Center for Ecological Environment in Arid Area
DOI | 10.2110/palo.2012.p12-042r |
THE PERMIAN-TRIASSIC TRANSITION IN THE CENTRAL COASTAL PLAIN OF ISRAEL (NORTH ARABIAN PLATE MARGIN), DAVID 1 BOREHOLE | |
Korngreen, Dorit1; Orlov-Labkovsky, Olga2; Bialik, Or1,3; Benjamini, Chaim3 | |
通讯作者 | Korngreen, Dorit |
来源期刊 | PALAIOS
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ISSN | 0883-1351 |
EISSN | 1938-5323 |
出版年 | 2013 |
卷号 | 28期号:7-8页码:491-508 |
英文摘要 | A succession that includes the Permian-Triassic transition was penetrated in the David 1 Borehole (Israel), located on the Levant margin sector of the northwestern Gondwanan plate. This is a fully marine section with a complex depositional interplay of distal siliciclastic and ramp carbonate sediment. Foraminifera distribution, sedimentary microfacies, delta C-13 excursions and e-log (gamma-ray; resistivity) data were analyzed. The local P-T boundary is placed at the first appearance of Triassic taxa, but there is a 90 m interval of overlapping faunas where the Permian taxa are small species atypical of the underlying Permian strata, and some specimens are clearly reworked. Carbonate strata were deposited in mid-to outer-ramp environments under varying conditions of sea level, storm regime, and siliciclastic (mostly silty) influx. Sea level, tracked by facies shifts, follows a low-order cyclic pattern. Two higher orders of cyclicity are also present: a short-term oscillation in storm frequency in the local depositional basin and a high-order mode in which clastic supply alternates with clastic-free carbonates, interpreted as reflecting humid-arid climate shifts of a remote, continental source region. The last mode lies within the Milankovich band of frequencies. Negative delta C-13 excursions, glauconite, and pyrite-rich horizons indicate hypoxic or anoxic conditions and reflect perturbations of the global carbon system in the oceans during this time. Although lithification of the latest Permian carbonates in the transitional interval was suppressed, the state of preservation of the carbonate components is not indicative of deposition under conditions of oceanic acidification. |
类型 | Article |
语种 | 英语 |
国家 | Israel |
收录类别 | SCI-E |
WOS记录号 | WOS:000329879000007 |
WOS关键词 | WESTERN UNITED-STATES ; ANACHRONISTIC CARBONATE FACIES ; EASTERN MEDITERRANEAN BASIN ; MASS EXTINCTION ; SOUTH CHINA ; OCEAN ACIDIFICATION ; FUNGAL EVENT ; SEQUENCE STRATIGRAPHY ; TECTONIC IMPLICATIONS ; PHANEROZOIC CYCLES |
WOS类目 | Geology ; Paleontology |
WOS研究方向 | Geology ; Paleontology |
来源机构 | Ben-Gurion University of the Negev |
资源类型 | 期刊论文 |
条目标识符 | http://119.78.100.177/qdio/handle/2XILL650/179156 |
作者单位 | 1.Geol Survey Israel, IL-95501 Jerusalem, Israel; 2.Tel Aviv Univ, Natl Museum Nat Hist, IL-69978 Tel Aviv, Israel; 3.Ben Gurion Univ Negev, IL-84105 Beer Sheva, Israel |
推荐引用方式 GB/T 7714 | Korngreen, Dorit,Orlov-Labkovsky, Olga,Bialik, Or,et al. THE PERMIAN-TRIASSIC TRANSITION IN THE CENTRAL COASTAL PLAIN OF ISRAEL (NORTH ARABIAN PLATE MARGIN), DAVID 1 BOREHOLE[J]. Ben-Gurion University of the Negev,2013,28(7-8):491-508. |
APA | Korngreen, Dorit,Orlov-Labkovsky, Olga,Bialik, Or,&Benjamini, Chaim.(2013).THE PERMIAN-TRIASSIC TRANSITION IN THE CENTRAL COASTAL PLAIN OF ISRAEL (NORTH ARABIAN PLATE MARGIN), DAVID 1 BOREHOLE.PALAIOS,28(7-8),491-508. |
MLA | Korngreen, Dorit,et al."THE PERMIAN-TRIASSIC TRANSITION IN THE CENTRAL COASTAL PLAIN OF ISRAEL (NORTH ARABIAN PLATE MARGIN), DAVID 1 BOREHOLE".PALAIOS 28.7-8(2013):491-508. |
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