New record of Bathonian-Callovian calcareous nannofossils in the eastern Karakoram block: a possible clue to understanding the dextral offset along the Karakoram Fault
We report the first record of Bathonian–Callovian calcareous nannofossils from a marine sedimentary sequence of the eastern Karakoram block, in northern India. The calcareous mudstones and packstones, occasionally bearing red chert nodules, yielded calcareous nanofossils and Middle Jurassic Choffati...
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| Published in | Terra nova (Oxford, England) Vol. 17; no. 2; pp. 149 - 157 |
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| Main Authors | , , |
| Format | Journal Article |
| Language | English |
| Published |
Oxford, UK
Blackwell Science Ltd
01.04.2005
Blackwell Publishing Ltd |
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| Abstract | We report the first record of Bathonian–Callovian calcareous nannofossils from a marine sedimentary sequence of the eastern Karakoram block, in northern India. The calcareous mudstones and packstones, occasionally bearing red chert nodules, yielded calcareous nanofossils and Middle Jurassic Choffatia furcula ammonoids. Middle to Upper Jurassic nannofossil assemblage is dominated by representatives of the genus Watznaueria. The occurrence of Ansulasphaera helvetica whose range is Upper Bathonian–Upper Callovian, indicates a correlation with nannofossil zones NJ12–13. The occurrence of Cyclagelosphaera wiedmannii further infer an Upper Bathonian–Callovian age. These specimens show affinities with those found in a similar sedimentary formation exposed in north Karakoram. This suggests the existence of a narrow and elongated sedimentary basin, oriented in a NW–SE direction, at a latitude of c. 25°–30°N. At that time, the Karakoram block was situated near the already welded Qiangtang block of Asia. The northern and eastern Karakoram blocks were connected during Middle Jurassic. The activity and dextral offset of the Karakoram fault separated the Jurassic sedimentary formations of the northern and eastern Karakoram blocks by c. 150 km. |
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| AbstractList | Abstract
We report the first record of Bathonian–Callovian calcareous nannofossils from a marine sedimentary sequence of the eastern Karakoram block, in northern India. The calcareous mudstones and packstones, occasionally bearing red chert nodules, yielded calcareous nanofossils and Middle Jurassic
Choffatia furcula
ammonoids. Middle to Upper Jurassic nannofossil assemblage is dominated by representatives of the genus
Watznaueria.
The occurrence of
Ansulasphaera helvetica
whose range is Upper Bathonian–Upper Callovian, indicates a correlation with nannofossil zones NJ12–13. The occurrence of
Cyclagelosphaera wiedmannii
further infer an Upper Bathonian–Callovian age. These specimens show affinities with those found in a similar sedimentary formation exposed in north Karakoram. This suggests the existence of a narrow and elongated sedimentary basin, oriented in a NW–SE direction, at a latitude of
c.
25°–30°N. At that time, the Karakoram block was situated near the already welded Qiangtang block of Asia. The northern and eastern Karakoram blocks were connected during Middle Jurassic. The activity and dextral offset of the Karakoram fault separated the Jurassic sedimentary formations of the northern and eastern Karakoram blocks by
c.
150 km. We report the first record of Bathonian-Callovian calcareous nannofossils from a marine sedimentary sequence of the eastern Karakoram block, in northern India. The calcareous mudstones and packstones, occasionally bearing red chert nodules, yielded calcareous nanofossils and Middle Jurassic Choffatia furcula ammonoids. Middle to Upper Jurassic nannofossil assemblage is dominated by representatives of the genus Watznaueria. The occurrence of Ansulasphaera helvetica whose range is Upper Bathonian-Upper Callovian, indicates a correlation with nannofossil zones NJ12-13. The occurrence of Cyclagelosphaera wiedmannii further infer an Upper Bathonian-Callovian age. These specimens show affinities with those found in a similar sedimentary formation exposed in north Karakoram. This suggests the existence of a narrow and elongated sedimentary basin, oriented in a NW-SE direction, at a latitude of c. 25 degrees-30 degrees N. At that time, the Karakoram block was situated near the already welded Qiangtang block of Asia. The northern and eastern Karakoram blocks were connected during Middle Jurassic. The activity and dextral offset of the Karakoram fault separated the Jurassic sedimentary formations of the northern and eastern Karakoram blocks by c. 150 km. [PUBLICATION ABSTRACT] We report the first record of Bathonian-Callovian calcareous nannofossils from a marine sedimentary sequence of the eastern Karakoram block, in northern India. The calcareous mudstones and packstones, occasionally bearing red chert nodules, yielded calcareous nanofossils and Middle Jurassic Choffatia furcula ammonoids. Middle to Upper Jurassic nannofossil assemblage is dominated by representatives of the genus Watznaueria. The occurrence of Ansulasphaera helvetica whose range is Upper Bathonian-Upper Callovian, indicates a correlation with nannofossil zones NJ12-13. The occurrence of Cyclagelosphaera wiedmannii further infer an Upper Bathonian-Callovian age. These specimens show affinities with those found in a similar sedimentary formation exposed in north Karakoram. This suggests the existence of a narrow and elongated sedimentary basin, oriented in a NW-SE direction, at a latitude of c. 25 degree -30 degree N. At that time, the Karakoram block was situated near the already welded Qiangtang block of Asia. The northern and eastern Karakoram blocks were connected during Middle Jurassic. The activity and dextral offset of the Karakoram fault separated the Jurassic sedimentary formations of the northern and eastern Karakoram blocks by c. 150 km. We report the first record of Bathonian–Callovian calcareous nannofossils from a marine sedimentary sequence of the eastern Karakoram block, in northern India. The calcareous mudstones and packstones, occasionally bearing red chert nodules, yielded calcareous nanofossils and Middle Jurassic Choffatia furcula ammonoids. Middle to Upper Jurassic nannofossil assemblage is dominated by representatives of the genus Watznaueria. The occurrence of Ansulasphaera helvetica whose range is Upper Bathonian–Upper Callovian, indicates a correlation with nannofossil zones NJ12–13. The occurrence of Cyclagelosphaera wiedmannii further infer an Upper Bathonian–Callovian age. These specimens show affinities with those found in a similar sedimentary formation exposed in north Karakoram. This suggests the existence of a narrow and elongated sedimentary basin, oriented in a NW–SE direction, at a latitude of c. 25°–30°N. At that time, the Karakoram block was situated near the already welded Qiangtang block of Asia. The northern and eastern Karakoram blocks were connected during Middle Jurassic. The activity and dextral offset of the Karakoram fault separated the Jurassic sedimentary formations of the northern and eastern Karakoram blocks by c. 150 km. |
| Author | Upadhyay, Rajeev Sinha, Anshu K Rai, Jyotsana |
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| Cites_doi | 10.1016/S0037-0738(96)00068-1 10.1007/978-94-011-4902-0_4 10.1016/0012-821X(96)00086-6 10.1098/rsta.1988.0135 10.1144/GSL.SP.2005.004.01.14 10.1046/j.1365-3121.1999.00259.x 10.1146/annurev.ea.15.050187.001241 10.1111/j.1365-3121.1990.tb00033.x 10.1144/jm.8.1.91 10.1007/978-3-642-78593-1_1 10.1144/GSL.MEM.1990.012.01.01 10.1016/S0031-0182(01)00409-6 |
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| References_xml | – start-page: 358 year: 1991 – volume: 167 start-page: 15 year: 1996 end-page: 28 article-title: Jurassic calcareous nannofossil biostratigraphy of western Europe. Compilation of recent studies and calibration of bioevents publication-title: Bull. Soc. Geol. – year: 1981 – start-page: 99 year: 1983 end-page: 106 – volume: 11 start-page: 278 year: 1999 end-page: 283 article-title: Discovery of Gondwana plant fossils and palynomorphs of Late Asselian (Early Permian) age in the Karakoram Block publication-title: Terra Nova – start-page: 196 year: 1980 – volume: 328 start-page: 33 year: 1999 end-page: 46 article-title: Contribution to the geology of the eastern Karakoram, India publication-title: Spec. Pap. Geol. Soc. 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| Snippet | We report the first record of Bathonian–Callovian calcareous nannofossils from a marine sedimentary sequence of the eastern Karakoram block, in northern India.... Abstract We report the first record of Bathonian–Callovian calcareous nannofossils from a marine sedimentary sequence of the eastern Karakoram block, in... We report the first record of Bathonian-Callovian calcareous nannofossils from a marine sedimentary sequence of the eastern Karakoram block, in northern India.... |
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| SubjectTerms | Ammonoidea Fossils Geological time Geology Sediments Watznaueria |
| Title | New record of Bathonian-Callovian calcareous nannofossils in the eastern Karakoram block: a possible clue to understanding the dextral offset along the Karakoram Fault |
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