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Journal articles on the topic 'Palynological analysis'

Author: Grafiati

Published: 10 March 2023

Last updated: 26 July 2025

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1

Ivanina, Antonina V. "Famenian palynostratigraphy of the Volyn–Podillya margin of the East–Europian platform." Вісник Дніпропетровського університету. Геологія, географія 26, no. 1 (2018): 71–78. http://dx.doi.org/10.15421/111808.

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Famenian carbonate-terrigenous deposits with thickness іn 300-580 m are widely distributed within the Volyn-Podillia margin of the East-European platform. It is the facies-varying complex of rocks, the stratification of which is very difficult because there are no faunal remains in the sediments (with the exception of the lower part). Therefore, during the study of this stratum, the palynological method and the palynostratigraphic division are very important. The main purposes of this study are to identify palynozones, distinguish their generalized description and to create a local scale of th

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2

Bunting, M. Jane, Barry G. Warner, and Clayton R. Morgan. "Interpreting pollen diagrams from wetlands: pollen representation in surface samples from Oil Well Bog, southern Ontario." Canadian Journal of Botany 76, no. 10 (1998): 1780–97. http://dx.doi.org/10.1139/b98-158.

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Pollen and spore analysis of surface sediment samples from 45 points within Oil Well Bog, a coniferous swamp near Cambridge, Ontario, was used to determine the possibility of identifying different wetland vegetation communities from their palynological record, and to assess the effects of variable wetland vegetation on the pollen representation of surrounding upland communities. The data obtained were mapped for individual taxa to allow direct comparison of the spatial patterns of vegetation abundance and the associated palynological assemblages, and cluster analysis was used to identify palyn

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3

Dimitrova, Tatyana. "Palynological analysis of the deposit Fosso Bianco, Central Italy." Geologica Balcanica 27, no. 1-2 (1997): 101–4. http://dx.doi.org/10.52321/geolbalc.27.1-2.101.

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The palynological analysis of the Fosso Bianco section is based on the data obtained from 23 samples. Most of the samples contain polydominant and very rarely monodominant forest components. The palynological documentation is based on a classification of some well-known paleoflora groups. The comparative characteristics of the pollen spectra are based mainly on the data of the boundary Pliocene/Pleistocene in Central Italy.

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Skvarla, John J., John R. Rowley, and Edward L. Vezey. "ANALYSIS OF THE THANIKAIMONI PALYNOLOGICAL INDICES." TAXON 38, no. 2 (1989): 233–36. http://dx.doi.org/10.2307/1220838.

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5

Barth, Ortrud Monika, and Cynthia Fernandes Pinto Da Luz. "Palynological analysis of Brazilian geopropolis sediments." Grana 42, no. 2 (2003): 121–27. http://dx.doi.org/10.1080/00173130310012512.

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6

Aira, M. J., H. Horn, and M. C. Seijo. "Palynological analysis of honeys from Portugal." Journal of Apicultural Research 37, no. 4 (1998): 247–54. http://dx.doi.org/10.1080/00218839.1998.11100979.

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7

de Oliveira, Marcelo Accioly Teixeira, Jorge Luis Porsani, Gisele Leite de Lima, Vivian Jeske-Pieruschka, and Hermann Behling. "Upper Pleistocene to Holocene peatland evolution in Southern Brazilian highlands as depicted by radar stratigraphy, sedimentology and palynology." Quaternary Research 77, no. 3 (2012): 397–407. http://dx.doi.org/10.1016/j.yqres.2011.12.006.

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Paleoenvironmental interpretation of proxy data derived from peatlands is largely based upon an evolutionary model for ombrotrophic bogs, in which peat accumulates in still environments. Reports on proxies obtained from minerotrophic fens, where hydrologic inputs are variable, are less common. In this study, a highland peatland in southern Brazil is presented through ground penetrating radar (GPR) and sedimentological, palynological and geochronologic data. The radar stratigraphic interpretation suggests a relatively complex history of erosion and deposition at the site since the beginning of

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8

Erica Oghaleoghene AKHUMI and Anthonia Nwaneze ASADU. "Palynostratigraphic Evaluation of Depositional Environment in Well E001 Niger Delta." International Journal of Science and Research Archive 13, no. 2 (2024): 2463–75. https://doi.org/10.30574/ijsra.2024.13.2.2391.

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Palynological investigation was carried out on E001 well to interpret the lithofacies and biostratigraphy with the aim of establishing the palynological zones and the consequent age, environment of deposition and paleoclimatic conditions of the rock sediments in the well, using visual microscopic observations to determine their lithological character and palynologic content of the sedimentary succession. E001 well is located on latitude 4° 31′ 16.58″N and longitude 8° 18′ 24.96″E onshore Niger Delta. The analysis of this study was carried out on 50 ditch cutting samples composite at 60ft inter

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9

Tripathi, S. K. M., and Divya Srivastava. "Palynological investigations, facies analysis and palaeoenvironmental interpretations from Late Palaeocene to Early Eocene lignites and associated sediments of Barmer, western India." Journal of Palaeosciences 59, no. (1-3) (2010): 1–32. http://dx.doi.org/10.54991/jop.2010.185.

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A lignite bearing sequence located in an open-cast mine near Banner, Rajasthan, western India, identified as Akli Formation is investigated for palynological and palynofacies studies. The palynoflora from about 13.5 mthick succession mainly comprised of clay, shale and lignite, composed of spore/pollen, dinoflagellate cysts and fungal remains, is dominated by angiospermic pollen particularly those showing affinity with the family Arecaceae. The succession, palynologically divisible into three zones, is dated as Thanetian to Ypresian in age. Studies on the dispersed organic matter isolated from

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10

Marquez, Gonzalo J., Marta A. Morbelli, and Gabriela E. Giudice. "Palynological analysis of Sphaeropteris gardneri (Cyatheaceae, Pteridophyta)." Anais da Academia Brasileira de Ciências 82, no. 2 (2010): 361–67. http://dx.doi.org/10.1590/s0001-37652010000200012.

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The spore morphology and wall ultrastructure of Sphaeropteris gardneri (Hook.) R.M. Tryon from Brazil were analyzed with LM, SEM and TEM. The spores are trilete with an ornamentation formed of short low ridges with spines in their margins. The exospore is 2.5μm thick, two- layered in section and single or branched channels are present. The perispore is 1.2μm thick and two-layered. The inner layer has three strata: the inner stratum is formed of a network of branched and fused threads, the middle stratum has threads with a radial orientation and in the outer stratum thin, dark fibres are immers

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11

Barth, Ortrud Monika, and Cynthia Fernandes Pinto da Luz. "Palynological analysis of Brazilian red propolis samples." Journal of Apicultural Research 48, no. 3 (2009): 181–88. http://dx.doi.org/10.3896/ibra.1.48.3.06.

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12

de Freitas, Alex da Silva, Ortrud Monika Barth, Érika de Oliveira Sales, Adriana Hitomi Matsuda, and Ligia Bicudo de Almeida-Muradian. "A palynological analysis of Brazilian propolis samples." Journal of ApiProduct and ApiMedical Science 3, no. 2 (2011): 67–74. http://dx.doi.org/10.3896/ibra.4.03.2.01.

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13

Orlóci, L., V. D. Pillar, and M. Anad. "Multiscale analysis of palynological records: new possibilities." Community Ecology 7, no. 1 (2006): 53–67. http://dx.doi.org/10.1556/comec.7.2006.1.6.

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14

Richard, Hervé. "Palynological Micro-Analysis in Neolithic Lake Dwellings." Journal of Archaeological Science 20, no. 3 (1993): 241–62. http://dx.doi.org/10.1006/jasc.1993.1017.

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15

Aleshinskaya, Anna, Anna Babenko, Maria Kochanova, and Alla Troshina. "Opportunities and Features of the Palynological Analysis Application on Various Types of Archaeological Sites." Stratum plus. Archaeology and Cultural Anthropology, no. 6 (December 30, 2021): 361–76. http://dx.doi.org/10.55086/sp216361376.

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A wide variety of archaeological sites associated with various human activity has led to the emergence of a wide range of problems solved by archaeological palynology. On the example of the palynological materials accumulated in the Laboratory of Nature Sciences of the Institute of Archaeology of the Russian Academy of Sciences, the opportunities and features of the palynological analysis application are considered both on classical objects for Russian archaeopalynology (cultural layer, buried soils, defensive ramparts, burial mounds, etc.) and on non-traditional ones (latrines, vessels, funer

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16

Lelono, Eko Budi. "PALYNOLOGICAL EVENTS OF THE TALANG AKAR FORMATION IN THE ON-SHORE AREA OF THE SOUTH SUMATRA BASIN." Scientific Contributions Oil and Gas 27, no. 2 (2022): 10–18. http://dx.doi.org/10.29017/scog.27.2.1049.

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South Sumatra has been well known as the one of the largest hydrocarbon producers in Indonesia. Due to its potentiality, South Sumatra has been explored since the Dutch era. Million barrels of oil have been pumped out from this area and many unpublished reports and papers have been made regarding the remaining reserve of this area. This study focuses on Talang Akar Formation which is considered as the main reservoir in South Sumatra. Talang Akar Formation is interpreted to be formed in a deltaic environment (De Coster, 1974). The deltaic sediment must have contained excellent palynomorph assem

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17

Eze, Emeka Lazarus, Kingsley Onyekwere Okengwu, and Geoffrey Chijioke Soronnadi-Ononiwu. "Paleoenvironment and Palynozonation of Osere-004 Well sequences, Niger Delta. Nigeria." Paleoenvironment and Palynozonation of Osere-004 Well sequences, Niger Delta. Nigeria 8, no. 11 (2024): 9. https://doi.org/10.5281/zenodo.10638273.

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Paleoenvironmental interpretation and palynozonation was carried out using fifty ditch cutting samples ranging from 7020 ft – 10020 ft, with a total thickness of 3000 m from Osere-004 Well. The lithology of the ditch cuttings was described and analysed using wet-sieving technique. Palynological sample preparation was also carried out on the ditch cuttings following the non-mineral acid method and was analysed using transmitting light microscope. The lithologic description  and wet-sieve analysis generated the lithology and sand- shale ratio/gradational plot. The palynological analys

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18

Lelono, Eko Budi. "Pollen Record Of Early/ Middle Miocene Boundary In The South Sumatra Basin." Scientific Contributions Oil and Gas 32, no. 2 (2022): 71–81. http://dx.doi.org/10.29017/scog.32.2.836.

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Early to Middle Miocene sediment obtained from three wells drilled in South Sumatera area has been evaluated for its micropaleontological content including foraminifera, calcareous nannoplankton and palynomorph. The boundary of Early/ Middle Miocene is clearly represented by zone N8/ N9 boundary based on foraminiferal analysis and zone NN4/ NN5 boundary on the basis of calcareous nannoplankton analysis. The rich assemblage of foraminifera and calcareous nannoplankton indicates the occurrence of marine sediment within the well sections. In addition, environmental markers of benthonic foraminife

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19

Nedashkovsky, Leonard, Maria Kochanova, Anna Aleshinskaya, and Elena Spiridonova. "Archaeobotanical Materials from the Golden Horde Settlements of the Saratov Volga Region." Vestnik Volgogradskogo gosudarstvennogo universiteta. Serija 4. Istorija. Regionovedenie. Mezhdunarodnye otnoshenija, no. 4 (August 2023): 94–106. http://dx.doi.org/10.15688/jvolsu4.2023.4.7.

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Introduction. The article considers archaeobotanical data obtained as a result of the analysis of plant macro- and microremains from the settlements of the Golden Horde epoch in the central part of the Saratov Volga region. Methods and materials. The results of the analyses of flotation samples allow us to obtain data on the plant food of the settled population. The interpretation of spore-pollen analyses allows us to trace the process of growth of the territory of monuments, the nature of the lands surrounding them, and the natural conditions and occupations of the population. Analysis. Finds

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20

Doláková, Nela. "Palynological Analysis Of Sediments From Za Hájovnou Cave." Acta Musei Nationalis Pragae Series B 70, no. 1-2 (2014): 35–42. https://doi.org/10.14446/AMNP.2014.35.

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Doláková, Nela (2014): Palynological Analysis Of Sediments From Za Hájovnou Cave. Acta Musei Nationalis Pragae Series B 70 (1-2): 35-42, DOI: 10.14446/AMNP.2014.35, URL: http://dx.doi.org/10.14446/amnp.2014.35

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21

Asadu, A. N., and V. O. Onowaro. "Palynomorph Biostratigraphy of VIC 97 Well, Nothern Depo Belt, Niger Delta, Nigeria." British Journal of Earth Sciences Research 11, no. 2 (2023): 1–15. http://dx.doi.org/10.37745/bjesr.2013/vol11n2115.

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Palynological and sedimentological studies were conducted on sixty ditch cutting rock samples from interval 460 to 4550 feets of VIC-97 well, located at OML 38, Northern Depo-belt, Niger-Delta, to delineate lithofacies units and the age of the rock succession. Standard methods of palynological sample analysis were used to disaggregate the palynomorphs from the rock matrix. Log signatures, sand/shale ratios, textural attributes, and accessory mineal compositions of ditch cutting rock samples were used as lithologic parameters to establish two lithofacies units; the transitional unit having a sa

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22

Morbelli, Marta A., and Irma G. Michelena. "Palynological analysis ofCheilanthesSpecies (Adiantaceae-Pteridophyta) of Northwestern Argentina." Grana 28, no. 4 (1989): 295–304. http://dx.doi.org/10.1080/00173138909427442.

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23

Scott, L., and C. B. Bousman. "Palynological analysis of hyrax middens from Southern Africa." Palaeogeography, Palaeoclimatology, Palaeoecology 76, no. 3-4 (1990): 367–79. http://dx.doi.org/10.1016/0031-0182(90)90121-m.

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24

Černjavska, Svetlana. "Palynological analysis of samples from the Padala Formation." Geologica Balcanica 30, no. 1-2 (2000): 18. http://dx.doi.org/10.52321/geolbalc.30.1-2.18.

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25

Horjan Zanki, Ivana, Dario Hruševar, and Božena Mitić. "Forensic potential of pollen grains: A case study from continental Croatia (town of Donja Stubica)." Periodicum Biologorum 125, no. 1-2 (2023): 15–25. http://dx.doi.org/10.18054/pb.v125i1-2.24327.

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Background and Purpose: Pollen grains can come as “ invisible” traces during forensic palynological expertise. As forensic palynology is not carried out in Croatia at all, the main aims of our work were to establish an initial palynological collection for a limited area in Croatia and determine its forensic potential. Materials and Methods: For our case study, we chose a typical town from continental Croatia, Donja Stubica, in which there had been no previous floristic studies. The field survey was conducted during 2005, 2007, and 2021. Floristic and palynological analysis was carried out with

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26

Trainor, Jessica, Jeffery Goodall, and Kathryn Amos. "Stratigraphy of the Birdrong: an integrated approach." APPEA Journal 52, no. 2 (2012): 684. http://dx.doi.org/10.1071/aj11098.

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A detailed study of the Early Cretaceous Birdrong Sequence (S. areolata - P. burgeri) has been undertaken in the East Spar and Woollybutt fields, which lie in the northern end of the Barrow Delta complex in the Barrow Sub-basin, Northern Carnarvon Basin. This project integrates palynological, sedimentological and seismic stratigraphic interpretations to progress our understanding of the way in which the Barrow Delta evolved. The results will help develop remaining hydrocarbon prospectivity in the northern Barrow area. Palynological analysis within the Helby, Morgan and Partridge (2004) zonatio

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27

Il'ina, N., and V. Zharkov. "Palynological assemblage of the Synya Formation (Middle Triassic) from outcrops at the Vertny river (Bol’shaya Synya Depression, the Timan-Northern Urals region)." Vestnik of geosciences, no. 3 (June 8, 2023): 23–41. http://dx.doi.org/10.19110/geov.2023.3.3.

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The results of a palynological study of terrigenous rocks exposed in the lower reaches of the Vertny River and correlated with the Syninskaya Formation of the Bolshesyninskaya Series of the Legend of the North Ural Sheet Series GK-200/2 are presented. The Middle Triassic (Ladinian) age of the rocks was determined. A quantitative analysis of the species composition of the identified palynological assemblage using the Sporomorph EcoGroup method (SEG-analysis) was carried out. Based on palynological data, elements of the vegetation cover and landscape conditions have been reconstructed. It is con

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28

Willems, Cees J. L., Andrea Vondrak, Dirk K. Munsterman, Marinus E. Donselaar, and Harmen F. Mijnlieff. "Regional geothermal aquifer architecture of the fluvial Lower Cretaceous Nieuwerkerk Formation – a palynological analysis." Netherlands Journal of Geosciences 96, no. 4 (2017): 319–30. http://dx.doi.org/10.1017/njg.2017.23.

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AbstractThe primary challenge for efficient geothermal doublet design and deployment is the adequate prediction of the size, shape, lateral extent and thickness (or aquifer architecture) of aquifers. In the West Netherlands Basin, fluvial Lower Cretaceous sandstone-rich successions form the main aquifers for geothermal heat exploitation. Large variations in the thickness of these successions are recognised in currently active doublet systems that cannot be explained. This creates an uncertainty in aquifer thickness prediction, which increases the uncertainty in doublet lifetime prediction as i

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29

Fadiya, S. L., S. O. Ogunleye, A. B. Oyelami, and F. R. Aroyewun. "Palynostratigraphic and palynofacies analysis of x and y wells, offshore Niger Delta, Nigeria." Ife Journal of Science 22, no. 3 (2021): 25–42. http://dx.doi.org/10.4314/ijs.v22i3.2.

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A detailed palynostratigraphic and palynofacies study was carried out on two shallow offshore wells, codenamed Well X and Well Y, from the Niger Delta Basin, Nigeria. The study is aimed at establishing the age and palaeoenvironment of the sedimentary sequences penetrated by the wells. Standard palynological/palynofacies laboratory procedures were used to free the palynomorphs and palynomacerals from the embedding matrices.Prepared palynological slides were studied using the Leitz Ortholux II transmitted light microscope. The palynofloral assemblages recorded from the two well sequences include

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30

Ferraz-vicentini, K. R., and M. L. Salgado-Labouriau. "Palynological analysis of a palm swamp in Central Brazil." Journal of South American Earth Sciences 9, no. 3-4 (1996): 207–19. http://dx.doi.org/10.1016/0895-9811(96)00007-7.

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31

Velázquez, Nadia Jimena, Lidia Susana Burry, and Martín Horacio Fugassa. "Palynological analysis of extinct herbivore dung from Patagonia, Argentina." Quaternary International 377 (August 2015): 140–47. http://dx.doi.org/10.1016/j.quaint.2015.05.012.

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32

Ganga, M., J. Lakshmi, N. Manivannan, and K. Rajamani. "Palynological investigations in Jasminum spp." Journal of Horticultural Sciences 15, no. 2 (2020): 183–90. http://dx.doi.org/10.24154/jhs.2020.v15i02.010.

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   The present investigation was carried out at the Department of Floriculture and Landscape Architecture, Horticultural College and Research Institute, Tamil Nadu Agricultural University, Coimbatore during 2017-2019. The study involved nine jasmine genotypes, four falling under the commercially cultivated types and five belonging to underutilized species or ‘lesser-known species’. The study was undertaken to investigate and document the palynological parameters of jasmines which could serve as a reliable reference for future jasmine breeding programmes. The palynological inv

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Ganga, M., J. Lakshmi, N. Manivannan, and K. Rajamani. "Palynological investigations in Jasminum spp." Journal of Horticultural Sciences 15, no. 2 (2020): 183–90. http://dx.doi.org/10.24154/jhs.v15i2.948.

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   The present investigation was carried out at the Department of Floriculture and Landscape Architecture, Horticultural College and Research Institute, Tamil Nadu Agricultural University, Coimbatore during 2017-2019. The study involved nine jasmine genotypes, four falling under the commercially cultivated types and five belonging to underutilized species or ‘lesser-known species’. The study was undertaken to investigate and document the palynological parameters of jasmines which could serve as a reliable reference for future jasmine breeding programmes. The palynological inv

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34

Madeja, Jacek, and Dariusz Latowski. "Too Old AMS Radiocarbon Dates Obtained from Moss Remains from Lake Kwiecko Bottom Sediments (N Poland)." Geochronometria 32, no. -1 (2008): 13–19. http://dx.doi.org/10.2478/v10003-008-0029-2.

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Too Old AMS Radiocarbon Dates Obtained from Moss Remains from Lake Kwiecko Bottom Sediments (N Poland)The paper presents the results of the AMS radiocarbon dating of moss macrofossils which seem to be too old in the context of palynological data. The lack of agreement between the obtained results of radiocarbon dating and pollen analysis has been discussed. Some possible causes of the discrepancies between the results of radiocarbon dating and palynological dating have been given.

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Goryacheva, A. A. "BIOSTRATIGRAPHY OF THE LOWER AND MIDDLE JURASSIC ACCORDING TO PALYNOLOGICAL DATA (THE TAIMYR PENINSULA, NORTH OF EASTERN SIBERIA)." Geology and mineral resources of Siberia, no. 3 (2023): 40–51. http://dx.doi.org/10.20403/2078-0575-2023-3-40-51.

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The article presents the results of palynological studies of the Lower-Middle Jurassic strata recovered from the Tulay-Kiryakskaya-1 well and represented by the Zimnyaya, Airkat, Kiterbyut, Korotkiy, Aprelevskiy, Arangastakh and Yuryung-Tumus Formations. The investigated well is situated on the territory of the Yana-Anabar facies region of marine sedimentogenesis. As a result of palynological analysis six biostratons with spores and pollen and four biostratons with dinocysts were established for the Pliensbachian-Bajocian interval and their geological age was substantiated.

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Singh, Vartika, and Sophia Barinova. "Palynological Analysis of Surface Sediments in a High Arctic Pond, Revealing Desmids as Indicators of Wetlands and Climate Change." Transylvanian Review of Systematical and Ecological Research 24, no. 1 (2022): 1–16. http://dx.doi.org/10.2478/trser-2022-0001.

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Abstract This is a first attempt to study the palynological remains from the surface sediments of a pond near the Kongsfjorden coast in Ny-Alesund, Svalbard, Norway. The palynomorphs display a high relative abundance of desmids, Cladocera, thecamoebians, chironomids, and fungal remains inherent to the inland aquatic ecosystem. The Cosmarium indicators characterize water as neutral pH, fresh, mesotrophic, without organic pollution, Class 2 of Water Quality as in wetlands with coastal vegetation. The single procedure of palynological analysis excluding the acetolysis step, and bioindicators allo

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Victoria, Okereke, and Ukpabi Ndubuisi. "Palynology and Palynofacies studies of fifteen shallow borehole samples from some parts of Delta and Bayelsa states, Niger Delta, Southern NIGERIA." International Journal of Innovation (IJInn) ISSN:0975 – 9808 8, no. 1 (2018): 1–11. https://doi.org/10.5281/zenodo.2494291.

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<strong>Title:</strong> Palynology and Palynofacies studies of fifteen shallow borehole samples from some parts of Delta and Bayelsa states, Niger Delta, Southern NIGERIA <strong>Authors & Affiliation:</strong> Victoria Okereke, Ndubuisi Ukpabi Geology Department, University of Port Harcourt, Rivers State. NIGERIA edgar2005ng@gmail.com, okerevicto@gmail.com <strong>ABSTRACT</strong> Rock Samples from fifteen shallow boreholes in some parts of Delta and Bayelsa states, Southern Nigeria was analysed for Palynology and Palynofacies studies to determine their paleoecology/paleoenvironment of d

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Lelono, Eko Budi. "Stratigraphic Interpretation Of The Middle Miocene Deltaic Sediment In The Sangatta Area, Based On Quantitative Palynological Data." Scientific Contributions Oil and Gas 26, no. 2 (2022): 2–16. http://dx.doi.org/10.29017/scog.26.2.876.

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This study demonstrates the ability of palynology in helping explorationist to comprehend the stratigraphic framework of the middle Miocene formation in the Sangatta area. Palynological analysis is performed on three different wells which are called X, Y and Z. With the exception of the samples situated in the lower part of the studied wells, most samples yield excellent palynomorph assemblages. High abundance of mangrove pollen suggests a good development of mangrove forest which indicates the occurrence of deltaic sediments within these three wells. The studied wells have been correlated bas

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Sirenko, Olena. "Correlation of the Upper Pliocene sediments of the Dnipro-Donetsk Depression based on palynological data." PROBLEMS OF GEOMORPHOLOGY AND PALEOGEOGRAPHY OF THE UKRAINIAN CARPATHIANS AND ADJACENT AREAS, no. 17 (December 15, 2024): 56–69. https://doi.org/10.30970/gpc.2024.2.4556.

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The problems of intra- and inter-regional correlations have always been the most difficult in stratigraphic studies. Particular difficulties arise when comparing same-age subaerial continental sediments that are depleted in palaeontological remains. The spore-pollen analysis, which is a component of the palynological method, is most effective in stratigraphic dissection and correlation of subaerial sediments, since pollen and spores, with few exceptions, are almost the only paleontological remains contained in fossil soils and intersoil clays and loess. The author has developed the methodologi

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40

Buratti, Nicoletta, Dorra Mehdi, Simonetta Cirilli, Fekri Kamoun, and Moncef Mzoughi. "A Carnian (Julian) microflora from the Djerba Melita 1 Borehole (Gulf of Gabes, South-Eastern Tunisia)." Micropaleontology 58, no. 4 (2012): 377–88. http://dx.doi.org/10.47894/mpal.58.4.05.

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This study represents a contribution to the biostratigraphic characterization of the Gulf of Gabes Triassic series. Diverse andwell preserved palynological assemblages from the Djerba Melita 1 (DJM1)well in the Djerba Island (Gulf ofGabes, Southern Tunisia) are here presented and discussed. A Carnian microflora is recorded in the Triassic portion of the drilled succession. The co-occurrence of Ladinian-lower Carnian taxa in association with typical Carnian elements allows to refer the microflora to the lower part of the Duplicisporites continuus palynological assemblage (late Julian, Austrotra

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Lelono, Eko Budi, and Robert J. Morley. "Oligocene Palynological Zonation Scheme From East Java Sea." Scientific Contributions Oil and Gas 34, no. 2 (2022): 95–104. http://dx.doi.org/10.29017/scog.34.2.797.

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Systematic biostratigraphic analyses have been undertaken on the Oligocene clastic and carbonate Kujung Formation from the East Java Sea, North of Madura. The succession has been examined mainly using cutting samples in two wells, using a combination of foraminiferal, nannofossil and palynological analyses at regular spacing. Nannofossil analysis indicates that the Late Oligocene to basal Early Miocene succession is more or less complete, with zones NP24, NP25 and NN1 are all being well developed. In addition, the Early Oligocene is indentified by larger foraminifera indicating the Tc/ Td Lett

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Bolikhovskaya, N. S., V. A. Ul’yanov, and M. V. Shun’kov. "PALYNOCLIMATOSTRATIGRAPHY AND FORMATION CONDITIO NS OF PLEISTOCENE DEPOSITS IN THE TRLICA CAVE (MONTENEGRO)." Lomonosov Geography Journal 78, no. 6 (2023) (2024): 107–18. http://dx.doi.org/10.55959/msu0579-9414.5.78.6.10.

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The results of palynological analysis allowed climatostratigraphic subdivision of Pleistocene deposits of the Trlica cave, located in the vicinity of Pljevlja town in northern Montenegro. The palynological record confirms significant hiatuses in the sedimentation revealed by the field lithologic-genetic analysis. The changes of landscape and climatic conditions that occurred during the formation of the studied Pleistocene strata are reconstructed. Specific features of flora and vegetation of three stages of the final part of the Early Pleistocene corresponding to MIS 22, MIS 21, MIS 20, as wel

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Fukuda, Tomoko, and Hiroshi Ikeda. "Palynological analysis and taxonomic position of the genus Mertensia (Boraginaceae)." Botany 90, no. 8 (2012): 722–30. http://dx.doi.org/10.1139/b2012-024.

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Palynological analysis of the genus Mertensia Roth, s. lat. (Boraginaceae) was performed. All pollen grains studied were mostly dumbbell shaped and had 6-heteroaperturate pollen type without exception. The type of pollen of Mertensia does not contradict recent classifications that assign Mertensia to Cynoglosseae. Among six sections of Mertensia, pollen grains of section Oreocharis (the Himalayan Mertensia) were different from those of other sections in having granulate sculpturing on the colpus and pseudocolpus membranes. The results, along with other morphological differences, may support Ri

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Reis, Carina I. C., Maria João Coimbra-Dores, Maria Teresa Rebelo, and Mafalda S. Faria. "Palynological analysis of soil in Portugal: potential for forensic science." Palynology 43, no. 4 (2018): 585–95. http://dx.doi.org/10.1080/01916122.2018.1503199.

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Sihombing, F. M. H., S. Sirait, A. Purnomo, D. Sulistiowati, and T. L. Indra. "Palynological analysis to infer environmental dynamics of Muarajambi Temple compound." IOP Conference Series: Earth and Environmental Science 538 (July 29, 2020): 012053. http://dx.doi.org/10.1088/1755-1315/538/1/012053.

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Arguelles, Paulette, Karl Reinhard, and Dong Hoon Shin. "Forensic Palynological Analysis of Intestinal Contents of a Korean Mummy." Anatomical Record 298, no. 6 (2015): 1182–90. http://dx.doi.org/10.1002/ar.23141.

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Istiana, M. G. Rachman, J. E. Ardine, I. D. Mustav, F. D. S. Alfinna, and M. Rohaman. "Stratigraphy of Jaten Formation based on palynology and sedimentology analysis in Dongko Area, Trenggalek, East Java." IOP Conference Series: Earth and Environmental Science 1339, no. 1 (2024): 012006. http://dx.doi.org/10.1088/1755-1315/1339/1/012006.

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Abstract Jaten Formation is located in the Southern Mountains of the eastern part of Java island. East Java is known as one of the largest provinces in Indonesia for oil and gas production. However, the exploited areas have primarily been in the northern part of East Java. The Southern Mountains region shows several indications of potential oil systems, such as shale outcrops in the Jaten Formation. This research aims to understand the stratigraphic characteristics of the Jaten formation using a palynological and sedimentological analysis approach. The palynological analysis result determined

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Maissuradze, Lamara, Irina Shatilova, Mzia Vekua, Kakhaber Koiava, Irma Kokolashvili, and Luara Rukhadze. "The Results of Micropaleontological Analysis of the Late Meotian-Early Pontian Deposits of the Black Sea Region." Proceedings of the Georgian National Museum, Natural Sciences and Prehistory Section 5 (December 25, 2013): 68–75. https://doi.org/10.5281/zenodo.1164624.

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The results of microfaunistical and palynological analysis of the Late Meotian - Early Pontian deposits of Eastern part of the Black Sea region are presented in the work. The data on the mollusks fauna studied from the same deposits were also used.

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Zhou, Zihan, Dangpeng Xi, Lixin Sun, et al. "Late Cretaceous (Santonian to Campanian) Palynological Records and Paleoclimatic Significance from Borehole ZKY2-1, Songliao Basin." Minerals 13, no. 3 (2023): 338. http://dx.doi.org/10.3390/min13030338.

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The global temperature gradually decreased from the Cretaceous Santonian to Campanian, while angiosperms evolved rapidly and gradually became dominant. The Songliao Basin, NE China, contains abundant fossil palynomorphs from the Santonian to Campanian age. A thorough investigation of fossil palynomorphs in borehole ZKY2-1 of the SW Songliao Basin was performed, reconstructing the vegetation and paleoclimate transition from the Santonian–earliest Campanian (lower Nenjiang Formation) to the late Campanian (Sifangtai Formation). Eighty form-genera from borehole ZKY2-1 have been identified. Three

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Nenasheva, G. I., M. S. Ivanova, N. S. Malygina та T. M. Kopytina. "Палинологическая характеристика медов Алтайского края". Ukrainian Journal of Ecology 7, № 4 (2017): 56–64. http://dx.doi.org/10.15421/2017_87.

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<p>The present paper contains results of the palynological research in Altai Territory which takes first place in the Siberian Region and fourth place in Russia in honey production. The development of criteria of the palynological authenticity of Altai honey is of great practical importance, since beekeeping is one of the priority directions of the of the region's economy development. We studied the honey resources of the mountain forest (Charysh, Soloneshnoe and Altaiskoe Districts), foothills-forest steppe (Smolenskoe District) and pinery (Pervomaiskoe District) zones of Altai Territor

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