Integrated sedimentological and palynological analysis from Early Cretaceous estuarine deposits in the southern-central Neuquén Basin, Argentina
The Mulichinco Formation represents one of the main gas producer unit in the Neuquén Basin and particularly, an improvement in its reservoir qualities are mostly indicated in subsurface for its upper section. Because the economic importance of this interval, sedimentological and palynological analys...
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2019
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| LEADER | 35699caa a22019817a 4500 | ||
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| 001 | PAPER-25572 | ||
| 003 | AR-BaUEN | ||
| 005 | 20230518205738.0 | ||
| 008 | 190410s2019 xx ||||fo|||| 00| 0 eng|d | ||
| 024 | 7 | |2 scopus |a 2-s2.0-85063288452 | |
| 040 | |a Scopus |b spa |c AR-BaUEN |d AR-BaUEN | ||
| 100 | 1 | |a Olivo, M.S. | |
| 245 | 1 | 0 | |a Integrated sedimentological and palynological analysis from Early Cretaceous estuarine deposits in the southern-central Neuquén Basin, Argentina |
| 260 | |b Elsevier Ltd |c 2019 | ||
| 270 | 1 | 0 | |m Olivo, M.S.; Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires, Universidad de Buenos Aires - CONICET, Ciudad Universitaria, Intendente Güiraldes 2160, Pabellón II, Piso 1, Argentina; email: olivomariana@gmail.com |
| 506 | |2 openaire |e Política editorial | ||
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| 520 | 3 | |a The Mulichinco Formation represents one of the main gas producer unit in the Neuquén Basin and particularly, an improvement in its reservoir qualities are mostly indicated in subsurface for its upper section. Because the economic importance of this interval, sedimentological and palynological analysis were made on deposits from outcrops of the upper section of the unit, located at the southern-central Neuquén Basin. The studied section includes four main facies association which represent accumulations in a wave-dominated estuary, non-previously described for the Mulichinco Formation in the study area. In addition, sixty-six new palynomorphs species were identified which were new for the unit, including fifty-six spore species, twenty-five pollen grain taxa, and two algae. Ferns and conifers species were identified as dominant taxa. Moreover, mega and palynofloristic assemblages provide information about drainage conditions of the inhabited environment, suggesting spatial variations when comparing upland subaerial well-drained plains with lowland subaqueous poorly-drained areas and, at the same time, climatic variations are considered, inferring temperate to warm and wet palaeoclimatic conditions. The integration of sedimentological and palynological interpretations provides a more complete picture of the Valanginian estuarine system and ecosystem that developed towards the southern-central area of the Neuquén Basin. Furthermore, the studied palynological assemblages are consistent with a Late Valanginian age, and can be referred to the Zone 2 and to the Cyclusphaera psilata-Classopollis Association suggested for the Neuquén Basin. © 2019 Elsevier Ltd |l eng | |
| 536 | |a Detalles de la financiación: PIP 11/N767, PIP 112-201101-00322 | ||
| 536 | |a Detalles de la financiación: Universidad Nacional de La Plata | ||
| 536 | |a Detalles de la financiación: PIP 0512 | ||
| 536 | |a Detalles de la financiación: PIP 0286 | ||
| 536 | |a Detalles de la financiación: Consejo Nacional de Investigaciones Científicas y Técnicas | ||
| 536 | |a Detalles de la financiación: Part of this work was developed during M. Olivo PhD work, which was developed in the Centro de Investigaciones Geológicas (CONIECT – UNLP) and funded by a postgraduate fellowship from the CONICET . CONICET and an agreement between National University of La Plata and YPF S.A. supported field work activities. We would like to thank Gualmes and Garrido families and Drs. L. C. A Martínez, A. Argüello Scotti and R. I. Escobar for their help assistance during fieldwork and collection of samples. The authors thank Dr. A. Carignano (School of Natural Sciences and Museum, National University of La Plata) for their assistance provided in identifying ostracods species. Thanks are extended to V. Guler for her help identifying the dinoflagellate cysts. We kindly thank Dr. D. Batten and anonymous reviewers of Palaios and Journal of South American Earth Sciences journals, whose comments and suggestions greatly improved this work. Finally, we are grateful to S. Mirabelli from the Museo Argentino de Ciencias Naturales for technical assistance in sample processing. This investigation was supported by the Projects CONICET PIP 0512, CONICET PIP 0286, CONICET PIP 112-201101-00322 and UNLP PIP 11/N767. Appendix A | ||
| 593 | |a Instituto de Geociencias Básicas, Aplicadas y Ambientales de Buenos Aires, Universidad de Buenos Aires - CONICET, Ciudad Universitaria, Intendente Güiraldes 2160, Pabellón II, Piso 1, Ciudad Autónoma de Buenos Aires, CP 1428, Argentina | ||
| 593 | |a Museo Argentino de Ciencias Naturales, “B. Rivadavia” - CONICET, Av. Ángel Gallardo 470, Ciudad de Buenos Aires, Argentina | ||
| 690 | 1 | 0 | |a ESTUARINE SYSTEM |
| 690 | 1 | 0 | |a PALAEOECOLOGY |
| 690 | 1 | 0 | |a PALYNOLOGY |
| 690 | 1 | 0 | |a SEDIMENTOLOGY |
| 690 | 1 | 0 | |a VALANGINIAN |
| 651 | 4 | |a NEUQUEN BASIN | |
| 700 | 1 | |a RombolA, C. | |
| 700 | 1 | |a Perez Loinaze, V.S. | |
| 700 | 1 | |a Kietzmann, D.A. | |
| 773 | 0 | |d Elsevier Ltd, 2019 |g v. 92 |h pp. 246-264 |p J. South Am. Earth Sci. |x 08959811 |w (AR-BaUEN)CENRE-1080 |t Journal of South American Earth Sciences | |
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| 856 | 4 | 0 | |u https://doi.org/10.1016/j.jsames.2019.02.022 |y DOI |
| 856 | 4 | 0 | |u https://hdl.handle.net/20.500.12110/paper_08959811_v92_n_p246_Olivo |y Handle |
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