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New planktonic foraminiferal record across the Aptian-Albian transition in Interior Fars, Zagros Basin, SW Iran: Implication for latest Aptian paleogeography along the southern shallower Neo-Tethys q
被引:1
|作者:
Sharifi, Javad
[1
]
Vahidinia, Mohammad
[1
]
Ando, Atsushi
[2
,3
]
Mahmudy-Gharaie, Mohamad Hosein
[1
]
机构:
[1] Ferdowsi Univ Mashhad, Fac Sci, Dept Geol, Mashhad, Iran
[2] Smithsonian Inst, Dept Paleobiol, Natl Museum Nat Hist, Washington, DC USA
[3] BugWare Inc, Tallahassee, FL USA
来源:
关键词:
Aptian-Albian;
Biostratigraphy;
Planktonic foraminifera;
Paleogeography;
Fars Platform;
Saroie section;
FOLD-THRUST BELT;
ANOXIC EVENT 1B;
SEA-LEVEL;
CARBONATE-PLATFORM;
KAZHDUMI FORMATION;
ARABIAN PLATE;
EVOLUTION;
SECTION;
STRATIGRAPHY;
SEDIMENTARY;
D O I:
10.1016/j.geobios.2023.05.005
中图分类号:
Q91 [古生物学];
学科分类号:
0709 ;
070903 ;
摘要:
The Aptian-Albian (A-A) transition encompassed a critical timing in the evolution of Fars Platform (Zagros Basin, SW Iran), such that a number of previous studies on its proximal part (called ''Coastal Fars") illustrated platform recovery after sustained demise due to latest Aptian maximum sea-level low-stand. So far, much less attention has been given to the distal part of the platform - ''Interior Fars" - where the lack of proper geological age interpretations, in particular, has been limiting a full paleoenvi-ronmental reconstruction of the southern shallower Neo-Tethys. In order to establish the chronostrati-graphic framework of Interior Fars, this study presents a novel set of planktonic foraminiferal record for the A-A Kazhdumi Formation at the Saroie section. The identified fauna comprises nine species from four genera, all of which are reported for the first time from Fars Platform. The observed new bioevents are generally consistent with those of the proposed reference section at a deeper intrashelf setting (Tang-e-Maghar, Dezful Embayment), allowing for the establishment of a local upper Aptian-Lower Albian zonation and leading to adequate constraints on the local Aptian/Albian boundary and the timing of prominent black shale deposition (possible ''Jacob" equivalent). Based on this new Saroie chronostrati-graphic scheme, it is evident that sedimentation across the A-A transition was maintained fully marine at the Saroie section, Interior Fars. This finding does not support the previous inference of extensive sub-aerial exposure of the entire Fars Platform at that time, thereby calling for a major revision of the pub-lished prevailing model for latest Aptian paleogeography of this region. These new insights will facilitate better understanding of the Fars Platform evolution in the Zagros Basin as well as paleoenviron-mental reconstructions along the southern Neo-Tethys.& COPY; 2023 Published by Elsevier Masson SAS.
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页码:49 / 62
页数:14
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