Western Tethyan Epeiric Ramp Setting in the Early Triassic:An Example from the Central Dinarides (Croatia)

Dunja Aljinović; Micha Horacek; Leopold Krystyn; Sylvain Richoz; Tea Kolar-Jurkovšek; Duje Smirčić; Bogdan Jurkovšek

doi:10.1007/s12583-018-0787-3

Volume 29 Issue 4

Jul 2018

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Journal of Earth Science > 2018 > 29(4): 806-823.

Dunja Aljinović, Micha Horacek, Leopold Krystyn, Sylvain Richoz, Tea Kolar-Jurkovšek, Duje Smirčić, Bogdan Jurkovšek. Western Tethyan Epeiric Ramp Setting in the Early Triassic:An Example from the Central Dinarides (Croatia). Journal of Earth Science, 2018, 29(4): 806-823. doi: 10.1007/s12583-018-0787-3

Citation:

Dunja Aljinović, Micha Horacek, Leopold Krystyn, Sylvain Richoz, Tea Kolar-Jurkovšek, Duje Smirčić, Bogdan Jurkovšek. Western Tethyan Epeiric Ramp Setting in the Early Triassic:An Example from the Central Dinarides (Croatia). Journal of Earth Science, 2018, 29(4): 806-823. doi: 10.1007/s12583-018-0787-3

Citation:

Dunja Aljinović, Micha Horacek, Leopold Krystyn, Sylvain Richoz, Tea Kolar-Jurkovšek, Duje Smirčić, Bogdan Jurkovšek. Western Tethyan Epeiric Ramp Setting in the Early Triassic:An Example from the Central Dinarides (Croatia). Journal of Earth Science, 2018, 29(4): 806-823. doi: 10.1007/s12583-018-0787-3

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Western Tethyan Epeiric Ramp Setting in the Early Triassic:An Example from the Central Dinarides (Croatia)

doi: 10.1007/s12583-018-0787-3

1.
University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Pierottijeva 6, Zagreb 10000, Croatia
2.
BLT Wieselburg, HBLFA Francisco-Josephinum, Rottenhauserstr. 1, Wieselburg 3250, Austria
3.
Institute of Paleontology, Vienna University, Althanstraße 14, Vienna 1090, Austria
4.
Lund University, Lithosphere and Biosphere science, Sölvegatan 12, Lund 22362, Sweden
5.
Geological Survey of Slovenia, Dimičeva Ulica 14, Ljubljana 1000, Slovenia

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Corresponding author: Duje Smirčić
Received Date: 27 Jul 2017
Accepted Date: 29 Mar 2018
Publish Date: 01 Aug 2018

Abstract

Abstract

In the central part of the External Dinarides in Plavno, Croatia, near Knin, a remarkably thick (927.5 m) Early Triassic depositional sequence was investigated. The Plavno sequence starts in the EarlyGriesbachian and ends with a continuous transition into the Anisian strata. A complete ¹³C isotope curve has been achieved and combined with conodonts, bivalves and ammonoids to establish and correlate stage and substage boundaries. The δ¹³C curve is consistent with former studies. It displays a general increase from the Griesbachian to a prominent maximum beyond the +8‰ amplitude around the Dienerian-Smithian boundary (DSB), followed by a steep and continuous decline to low, negative values in the Smithian. Around the Smithian-Spathian boundary (SSB) a steep rise to a second maximum occurred. It is followed by a saw-tooth shaped decline in the Spathian and a similar increase to a peak at the Spathian-Anisian boundary (SAB).Sedimentologically, the Plavno sequence is interpreted as having been deposited on an extensive epeiric ramp under long-term transgressive conditions, sharing depositional characteristics of both the epeiric platform and the carbonate ramp. The entire Plavno sequence was deposited above the storm-wave base and was storm influenced. Three informal members are differentiated:1) the dolo-stone member (Early Griesbachian); 2) the siliciclastic member (red-coloured shale, siltstone, sand-stone with oolitic/bioclastic grainstone intercalations), which can be further divided into lower, mid-dle and upper intervals (Late Griesbachian, Dienerian and Smithian); and 3) the mudstone member (grey lime mudstones, marls and calcisiltites with common ammonoids and gastropods-Spathian). The Plavno sequence is compared with other western Tethyan sections. Observed differences stem from local controls on deposition in the overall shallow marine environment.
- Early Triassic,
- Dinarides,
- epeiric ramp,
- δ¹³C isotope curve,
- litho-and biostratigraphy

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References(107)

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