Paleocene orthophragminids from the Lakadong Limestone, Mawmluh Quarry section, Meghalaya (Shillong, NE India): implications for the regional geology and paleobiogeography

IF 4.1 3区 地球科学 Q1 PALEONTOLOGY Journal of Micropalaeontology Pub Date : 2018-04-18 DOI:10.5194/JM-37-357-2018
E. Özcan, J. Pignatti, Christer Dominique Pereira, A. O. Yücel, K. Drobne, F. Barattolo, P. Saraswati
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引用次数: 14

Abstract

Abstract. The late Paleocene orthophragminids, hitherto poorly known from the Himalayan foreland basins, are studied from the Lakadong Limestone in Meghalaya, northeastern India, in order to establish a systematic, biostratigraphic, and paleobiogeographical framework for them in the eastern Tethys. In the Mawmluh Quarry section (MQS) on the Shillong Plateau, to the southeast of Tibet, orthophragminids are associated with typical Paleocene orbitoidiform taxa endemic to the Indian subcontinent, i.e., Lakadongia Matsumaru & Jauhri ( =  Setia Ferrandez-Canadell) and Orbitosiphon Rao, and various species of alveolinids, miscellaneids, and rotaliids, characterizing the Shallow Benthic Zones (SBZ) 3 and 4. The orthophragminids belong to two lineages of the genus Orbitoclypeus Silvestri: O. schopeni (Checchia-Rispoli) and O. multiplicatus (Gumbel), both well known from the peri-Mediterranean region and Europe (western Tethys). The latter species is identified here for the first time from the eastern Tethys. Previous records of the genus Discocyclina Gumbel from the Lakadong Limestone actually correspond to misidentified Orbitoclypeus; this implies that the late Paleocene orthophragminid assemblages from Meghalaya and eastern Tethys were less diverse than in the western Tethys. The lineage of Orbitoclypeus schopeni in the lower part of the Lakadong Limestone (SBZ 3) is identified as O. schopeni cf. ramaraoi based on the morphometry of a few specimens, whereas in the upper part (SBZ 4) it corresponds to a transitional development stage between O. schopeni ramaraoi and O. schopeni neumannae (with average Dmean values ranging between 192 and 199  µm ). The embryon diameters of O. multiplicatus, recorded only in SBZ 4, range between 300 and 319  µm on average, corresponding to transitional development stages of O. multiplicatus haymanaensis and O. multiplicatus multiplicatus. Our data, along with a review of previous Paleocene and Eocene records from India and Pakistan, suggest that Orbitoclypeus is the only orthophragminid in the Paleocene of the eastern Tethys, whereas Discocyclina first appears in early Eocene times, being mainly represented by endemic taxa confined to the Indian subcontinent. Facies change in the MQS from a marine to continental setting within SBZ 4 corresponds to the oldest record from the Indian plate in the Paleogene, which may be linked to the flexural uplift of the passive margin of the Indian plate, marking the onset of the collision of the Indian and Eurasian plates.
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Meghalaya(Shillong,NE India)Mawmluh采石场Lakadong石灰岩中的古新世直翅目:对区域地质和古生物地理学的影响
摘要研究了印度东北部Lakadong Limestonein Meghalaya的古新世晚期的正hragminids,迄今为止在喜马拉雅前陆盆地中鲜为人知,目的是为它们在东部地区建立一个系统的、生物地层学和古生物地理学框架。在西藏东南部Shillong高原的Mawmluh采石场区(MQS),直翅目昆虫与印度次大陆特有的典型古新世或类化石分类群有关,即Lakadongia Matsumaru和Jauhri(= SetiaFerrandez-Canadell)和Orbitosiphon Rao,以及各种类型的肺泡类、杂球藻类和轮状体,表征了浅海底带(SBZ)3和4。这些直齿目动物属于Orbitoclypus Silvestri属的两个谱系:O.schopeni(Checchia Rispoli)和O.multipliccatus(Gumbel),这两个谱系在地中海沿岸地区和欧洲(特提斯西部)都很有名。后一个物种是首次在东地中海发现的。拉卡洞石灰岩中盘环孢属的先前记录实际上对应于错误识别的Orbitocypeus;这意味着,来自梅加拉亚和特提斯东部的古新世晚期的正射虫群落的多样性不如特提斯西部。拉卡洞石灰岩下部(SBZ3)的Orbitoclypus schopeni谱系被鉴定为O.schopeni。根据少数标本的形态计量学,ramaraoi,而在上部(SBZ4),它对应于O之间的过渡发育阶段。schopeni ramaraoi和O.schopeni neumannae(平均D均值在192和199之间  µm)。仅在SBZ 4中记录到的多倍体O.multiplicatus的胚胎密度在300到319之间  平均µm,对应于海马纳O.multiplicatus haymanaensis和O.multipliccatus multipliccattus的过渡发育阶段。我们的数据,以及对印度和巴基斯坦以前的古新世和始新世记录的回顾表明,Orbitoclypusis是特提斯东部古新世唯一的直齿目动物,Discocyclina首次出现在始新世早期,主要由局限于印度次大陆的特有类群代表。SBZ 4内MQS从海洋环境到大陆环境的相变化对应于古近系印度板块的最古老记录,这可能与印度板块被动边缘的弯曲隆起有关,标志着印度板块和欧亚板块碰撞的开始。
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来源期刊
Journal of Micropalaeontology
Journal of Micropalaeontology 生物-古生物学
CiteScore
4.30
自引率
5.00%
发文量
7
审稿时长
>12 weeks
期刊介绍: The Journal of Micropalaeontology (JM) is an established international journal covering all aspects of microfossils and their application to both applied studies and basic research. In particular we welcome submissions relating to microfossils and their application to palaeoceanography, palaeoclimatology, palaeobiology, evolution, taxonomy, environmental change and molecular phylogeny.
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