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Artículos de revistas sobre el tema "Palynology"

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Autor: Grafiati

Publicado: 4 de junio de 2021

Última modificación: 31 de julio de 2024

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1

Mildenhall, D. C., P. E. J. Wiltshire y V. M. Bryant. "Forensic palynology". Forensic Science International 163, n.º 3 (noviembre de 2006): 161–62. http://dx.doi.org/10.1016/j.forsciint.2006.07.013.

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2

Edwards, Kevin J. "Quaternary palynology". Progress in Physical Geography: Earth and Environment 10, n.º 1 (marzo de 1986): 81–99. http://dx.doi.org/10.1177/030913338601000105.

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3

van Zinderen Bakker, E. M. "Archaeology and Palynology". South African Archaeological Bulletin 50, n.º 162 (diciembre de 1995): 98. http://dx.doi.org/10.2307/3889058.

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4

de Andrade Vieira Filho, Claudio L., Mark Reilly, Suzanne Hurter y Zsolt Hamerli. "Integration of biostratigraphy into a sequence stratigraphic framework for the Surat Basin, eastern Australia". APPEA Journal 59, n.º 2 (2019): 863. http://dx.doi.org/10.1071/aj18071.

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A new sequence stratigraphic framework (SSF) for the Early–Late Jurassic Surat Basin, eastern Australia, is evolving. A second and third order framework based upon an integrated methodology of well-to-well correlations supported by well tied seismic data is being developed. The integration of an additional dataset (palynology) to test for regionally consistent sequence stratigraphic well correlations offers an improvement in defining sequence boundaries related to the geological timescale. The palynological data from 33 wells covering the north-east Surat Basin were extracted from the Queensland Digital Exploration (QDEX) open-file reports, some of which date back to the 1960s. These data were correlated and superposed on the SSF for age comparison. The dataset used in this study represents only a subset of all existing palynology information, as not all data are captured in QDEX. However, the palynology data in this exploratory study generally fits and supports the new SSF with only one exception, the reason for which is not understood at this stage. We recommend expanding this study to include more data because palynology can support stratigraphic interpretation, especially in wells that do not intercept, or have log data across, regional datums.

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5

Morton, Cynthia M., S. Nilsson y J. Praglowski. "Erdtman's Handbook of Palynology." Brittonia 45, n.º 4 (octubre de 1993): 345. http://dx.doi.org/10.2307/2807614.

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6

Agashe, Shripad N. "Palynology and its application". Journal of Palaeosciences 55, n.º (1-3) (31 de diciembre de 2006): 115–16. http://dx.doi.org/10.54991/jop.2006.100.

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7

Ferguson, I. K., Siwert Nilsson y Joseph Praglowski. "Erdtman's Handbook of Palynology". Kew Bulletin 48, n.º 3 (1993): 628. http://dx.doi.org/10.2307/4118734.

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8

Schmid, Rudolf, Siwert Nilsson, Joseph Praglowski y Erdtman. "Erdtman's Handbook of Palynology". Taxon 44, n.º 3 (agosto de 1995): 479. http://dx.doi.org/10.2307/1223446.

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9

Servais, Thomas, Jan Jansonius y D. Colin McGregor. "Palynology: Principles and Applications". Micropaleontology 43, n.º 3 (1997): 332. http://dx.doi.org/10.2307/1485834.

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10

Edwards, Kevin J., H. R. Delcourt y P. A. Delcourt. "For Palaeoecology Read Palynology". Journal of Biogeography 19, n.º 2 (marzo de 1992): 231. http://dx.doi.org/10.2307/2845511.

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11

Fahrenkamp-Uppenbrink, J. "How palynology was born". Science 354, n.º 6311 (27 de octubre de 2016): 429–31. http://dx.doi.org/10.1126/science.354.6311.429-q.

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12

McGregor, D. C. "Palynology—The International Connection". Grana 26, n.º 1 (abril de 1987): 5–10. http://dx.doi.org/10.1080/00173138709428900.

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13

Vandenbroucke, Thijs R. A., Marco Vecoli y Thomas Servais. "Palaeozoic applied marine palynology". Review of Palaeobotany and Palynology 198 (noviembre de 2013): 1. http://dx.doi.org/10.1016/j.revpalbo.2013.08.005.

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14

Méon, Henritte. "Palynology of arid lands". Geobios 27, n.º 1 (enero de 1994): 72. http://dx.doi.org/10.1016/s0016-6995(06)80213-5.

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15

Paudayal, Khum N. y David K. Ferguson. "Pleistocene palynology of Nepal". Quaternary International 117, n.º 1 (enero de 2004): 69–79. http://dx.doi.org/10.1016/s1040-6182(03)00117-4.

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16

Zelikson, Ella M. "Methodology of loess palynology". GeoJournal 36, n.º 2-3 (1995): 223–28. http://dx.doi.org/10.1007/bf00813174.

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17

Okoli, Bosa E. y B. L. Nyananyo. "Palynology ofTelfairia L. (Cucurbitaceae)". Folia geobotanica & phytotaxonomica 23, n.º 3 (diciembre de 1988): 281–83. http://dx.doi.org/10.1007/bf02854822.

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18

BERGLUND, BJÖRN E. "Tropical palynology and palaeoecology". Boreas 18, n.º 2 (16 de enero de 2008): 126. http://dx.doi.org/10.1111/j.1502-3885.1989.tb00382.x.

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19

Wiltshire, Patricia E. J. "Protocols for forensic palynology". Palynology 40, n.º 1 (26 de octubre de 2015): 4–24. http://dx.doi.org/10.1080/01916122.2015.1091138.

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20

Punt, W. "Erdtman's Handbook of Palynology". Review of Palaeobotany and Palynology 77, n.º 3-4 (junio de 1993): 305. http://dx.doi.org/10.1016/0034-6667(93)90010-r.

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21

Graham, Alan. "Palynology of arid lands". Review of Palaeobotany and Palynology 83, n.º 4 (octubre de 1994): 351–52. http://dx.doi.org/10.1016/0034-6667(94)90145-7.

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22

Viarchuk, A. N., S. V. Kubrak y A. V. Kilchevskiy. "TRENDS IN MODERN PALYNOLOGY AND PROSPECTS OF USING DNA BARCODING FOR THE DIFFERENTIATION OF PLANTS BY POLLEN". Молекулярная и прикладная генетика 31 (8 de diciembre de 2021): 134–46. http://dx.doi.org/10.47612/1999-9127-2021-31-134-146.

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Classical palynology is based on the morphological description of pollen obtained using the light microscopy technique, which has along with its advantages a number of limitations. Due to the genetic study of mixtures of pollen and spores of different plant species, it will be possible to obtain more accurate identification of pollen species composition and to replace or effectively supplement morphological analysis with DNA analysis. The presented literature review demonstrates great potential of using pollen DNA barcoding in a number of areas of applied palynology.

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23

王, 朋. "Sampling Methods in Palaeoclimatological Palynology". Hans Journal of Agricultural Sciences 11, n.º 04 (2021): 290–96. http://dx.doi.org/10.12677/hjas.2021.114043.

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24

Schoenwetter, James y Geoffrey W. Dimbleby. "The Palynology of Archaeological Sites". American Antiquity 52, n.º 1 (enero de 1987): 204. http://dx.doi.org/10.2307/281080.

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25

Lelono, Eko Budi. "Pleistocene Palynology Of East Java". Scientific Contributions Oil and Gas 29, n.º 3 (29 de marzo de 2022): 3–14. http://dx.doi.org/10.29017/scog.29.3.868.

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This study is a part of geological investigation on Pleistocene sediment in East Java in order to evaluate hydrocarbon potential within this sediment of this area. The area of study is located in the on-shore East Java (Figure 1). It is financially supported by the oil company as this is commercial work done by LEMIGAS Exploration Department. Therefore, data used in this paper will be incompletely presented as they are confidential. The name of the studied wells and their precise locations are hided in this paper. Data used in this study derives from three wells namely R, S and T. Three different disciplines are applied in this study including palynology, micropaleontology and nannoplankton analyses which are useful for crosschecking purposes. Apparently, the integration of these analyses gains accurate interpretation of stratigraphy and depositional environment. The area of study is in East Java Basin which can be classified as a classical back-arc basin. During Pleistocene, the area of study was marked by regional uplift and the cessation of open marine sedimentation (LEMIGAS, 2005). Therefore Pleistocene age was dominated by non-marine deposition. Generally, this type of sediment is separated from the underlying layer by an unconformity (LEMIGAS, 2005). Most Pleistocene sediment consists of volcanoclastic as a result of volcanic activity which related to uplifting period. It is possible that volcanic activity was responsible for the burning of grass as indicated by the occurrence of charred Gramineae cuticles.

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26

Huntley, J. P. y G. W. Dimbleby. "The Palynology of Archaeological Sites." Journal of Ecology 74, n.º 2 (junio de 1986): 600. http://dx.doi.org/10.2307/2260278.

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27

HALL, ANTHONY V. "Systematic palynology of the Bruniaceae". Botanical Journal of the Linnean Society 96, n.º 3 (marzo de 1988): 285–96. http://dx.doi.org/10.1111/j.1095-8339.1988.tb00684.x.

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28

MANGALY, JOSE K. y JYOTHI NAYAR. "Palynology of South Indian Zingiberaceae". Botanical Journal of the Linnean Society 103, n.º 4 (agosto de 1990): 351–66. http://dx.doi.org/10.1111/j.1095-8339.1990.tb00195.x.

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29

Berglund, Björn. "Quaternary palynology in eastern Europe". Boreas 33, n.º 2 (1 de junio de 2004): 182. http://dx.doi.org/10.1080/03009480310000000.

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30

Salgado-Labouriau, Maria Lea. "Palynology of the Venezuelan Andes". Grana 30, n.º 2 (enero de 1991): 342–49. http://dx.doi.org/10.1080/00173139109431989.

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31

Servais, Thomas y Charles Wellman. "New directions in Palaeozoic palynology". Review of Palaeobotany and Palynology 130, n.º 1-4 (julio de 2004): 1–15. http://dx.doi.org/10.1016/j.revpalbo.2004.01.001.

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32

Mildenhall, D. C. "Forensic palynology in New Zealand". Review of Palaeobotany and Palynology 64, n.º 1-4 (octubre de 1990): 227–34. http://dx.doi.org/10.1016/0034-6667(90)90137-8.

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33

Thiede, Jörn. "Northwest European Micropalaeontology and Palynology". Physics of the Earth and Planetary Interiors 66, n.º 3-4 (abril de 1991): 335–36. http://dx.doi.org/10.1016/0031-9201(91)90093-w.

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34

Hughes, Norman F. "Northwest European Micropalaeontology and palynology". Palaeogeography, Palaeoclimatology, Palaeoecology 91, n.º 1-2 (enero de 1992): 183–84. http://dx.doi.org/10.1016/0031-0182(92)90041-3.

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35

Norris, G. "Palynology and British Purbeck facies". Geological Magazine 122, n.º 2 (marzo de 1985): 187–90. http://dx.doi.org/10.1017/s0016756800031101.

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36

Babcock, Steven L. y Sophie Warny. "Forensic Palynology as Classroom Inquiry". Science Activities: Classroom Projects and Curriculum Ideas 51, n.º 4 (10 de septiembre de 2014): 116–28. http://dx.doi.org/10.1080/00368121.2014.931270.

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37

Janssens, Steven B., Stefan Vinckier, Katrien Bosselaers, Erik F. Smets y Suzy Huysmans. "Palynology of African Impatiens (Balsaminaceae)". Palynology 43, n.º 4 (12 de diciembre de 2018): 621–30. http://dx.doi.org/10.1080/01916122.2018.1509149.

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38

van Konijnenburg-van Cittert, J. H. A. "Northwest European micropalaeontology and palynology". Earth-Science Reviews 32, n.º 3 (abril de 1992): 209–11. http://dx.doi.org/10.1016/0012-8252(92)90043-s.

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39

Kumaran, Navnith K. P. y Ruta B. Limaye. "Holocene Palynology and Tropical Paleoecology". Quaternary International 325 (marzo de 2014): 1–2. http://dx.doi.org/10.1016/j.quaint.2014.02.005.

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40

Punt, W. "Northwest European Micropalaeontology and Palynology". Review of Palaeobotany and Palynology 74, n.º 1-2 (octubre de 1992): 159. http://dx.doi.org/10.1016/0034-6667(92)90143-5.

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41

Pilcher, J. R. "The palynology of archaeological sites". Journal of Archaeological Science 13, n.º 2 (marzo de 1986): 202. http://dx.doi.org/10.1016/0305-4403(86)90009-9.

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42

Lelono, Eko Budi. "PLEISTOCENE PALYNOLOGY OF EAST JAVA". Scientific Contributions Oil and Gas 29, n.º 3 (29 de marzo de 2022): 3–14. http://dx.doi.org/10.29017/scog.29.3.1027.

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This study is a part of geological investigation on Pleistocene sediment in East Java in order to evaluate hydrocarbon potential within this sediment of this area. The area of study is located in the on-shore East Java (Figure 1). It is financially supported by the oil company as this is commercial work done by LEMIGAS Exploration Department. Therefore, data used in this paper will be incompletely presented as they are confidential. The name of the studied wells and their precise locations are hided in this paper. Data used in this study derives from three wells namely R, S and T. Three different disciplines are applied in this study including palynology, micropaleontology and nannoplankton analyses which are useful for crosschecking purposes. Apparently, the integration of these analyses gains accurate interpretation of stratigraphy and depositional environment. The area of study is in East Java Basin which can be classified as a classical back-arc basin. During Pleistocene, the area of study was marked by regional uplift and the cessation of open marine sedimentation (LEMIGAS, 2005). Therefore Pleistocene age was dominated by non-marine deposition. Generally, this type of sediment is separated from the underlying layer by an unconformity (LEMIGAS, 2005). Most Pleistocene sediment consists of volcanoclastic as a result of volcanic activity which related to uplifting period. It is possible that volcanic activity was responsible for the burning of grass as indicated by the occurrence of charred Gramineae cuticles. The previous investigations on Pleistocene sediment showed the domination of grass pollen of Monoporites annulatus which suggested the expansion of dry climate during Pleistocene glacial maxima. The pollen diagram from Lombok Ridge produced by van der Kaas (1991a) proves the domination of Gramineae pollen during Pleistocene (Figure 2). The period of dry climate (glacial climate) is characterised by abundant Gramineae pollen, whilst the period of wetter climate (interglacial climate) is indicated by an increase of coastal and mangrove palynomorphs, but greatly reduced frequencies of Graminaae pollen (Morley, 2000). In addition, Rahardjo et al. (1994) referred to the high abundance of Monoporites annulatus to propose Pleistocene pollen zone of M. annulatus (Figure 3).

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43

Kong, Zhaochen, Yun Zhang, Li Wang, Xiaohong Duan y Yumei Li. "The past, present and future of palynology in China—Concentrate on Quaternary palynology". Chinese Science Bulletin 63, n.º 2 (29 de diciembre de 2017): 164–71. http://dx.doi.org/10.1360/n972017-00812.

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44

Veiga, Allan, Antonio Saraiva y Cláudia da Silva. "The Online Pollen Catalogs Network (RCPol)". Biodiversity Information Science and Standards 2 (17 de mayo de 2018): e25658. http://dx.doi.org/10.3897/biss.2.25658.

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Aiming at promoting interaction among researchers and the integration of data from their pollen collections, herbaria and bee collections, RCPol was created in 2013. In order to structure RCPol work, researchers and collaborators have organized information on Palynology and trophic interactions between bees and plants. During the project development, different computing tools were developed and provided on RCPol website (http://rcpol.org.br), including: interactive keys with multiple inputs for species identification (http://chaves.rcpol.org.br); a glossary of palinology related terms (http://chaves.rcpol.org.br/profile/glossary/eco); a plant-bee interactions database (http://chaves.rcpol.org.br/interactions); and a data quality tool (http://chaves.rcpol.org.br/admin/data-quality). Those tools were developed in partnership with researchers and collaborators from Escola Politécnica (USP) and other Brazilian and foreign institutions that act on palynology, floral biology, pollination, plant taxonomy, ecology, and trophic interactions. The interactive keys are organized in four branches: palynoecology, paleopalynology, palynotaxonomy and spores. These information are collaboratively digitized and managed using standardized Google Spreadsheets. All the information are assessed by a data quality assurance tool (based on the conceptual framework of TDWG Biodiversity Data Quality Interest Group Veiga et al. 2017) and curated by palynology experts. In total, it has published 1,774 specimens records, 1,488 species records (automatically generated by merging specimens records with the same scientific name), 656 interactions records, 370 glossary terms records and 15 institutions records, all of them translated from the original language (usually Portuguese or English) to Portuguese, English and Spanish. During the projectʼs first three years, 106 partners, among researchers and collaborators from 28 institutions from Brazil and abroad, actively participated on the project. An important part of the project's activities involved training researchers and students on palynology, data digitization and on the use of the system. Until now six training courses have reached 192 people.

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45

Budi 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, n.º 2 (30 de marzo de 2022): 2–16. http://dx.doi.org/10.29017/scog.26.2.995.

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46

Barth, Ortrud Monika y Léa Maria Medeiros Carreira. "Recent Palynology in Caxiuana, Pará, Brazil". OALib 03, n.º 05 (2016): 1–7. http://dx.doi.org/10.4236/oalib.1102684.

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47

Butterfield, Nicholas J. y John P. Grotzinger. "Palynology of the Huqf Supergroup, Oman". Geological Society, London, Special Publications 366, n.º 1 (2012): 251–63. http://dx.doi.org/10.1144/sp366.10.

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48

Holt, K. A. y K. D. Bennett. "Principles and methods for automated palynology". New Phytologist 203, n.º 3 (27 de mayo de 2014): 735–42. http://dx.doi.org/10.1111/nph.12848.

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49

Soladoye, Michael O. y Peter R. Crane. "Systematic palynology of Baphia (Sophoreae, Papilionoideae)". Grana 24, n.º 3 (diciembre de 1985): 145–60. http://dx.doi.org/10.1080/00173138509431003.

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50

Pacltová, Blanka. "Palynology of metamorphic rocks (methodological study)". Review of Palaeobotany and Palynology 48, n.º 4 (septiembre de 1986): 347–56. http://dx.doi.org/10.1016/0034-6667(86)90072-2.

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