Bibliografías temáticas / Palynology

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Literatura académica sobre el tema "Palynology"

Autor: Grafiati
Publicado: 4 de junio de 2021
Última modificación: 31 de julio de 2024

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Artículos de revistas sobre el tema "Palynology"

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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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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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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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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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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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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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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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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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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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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Tesis sobre el tema "Palynology"

1

Seetharam, Y. N. "Clusiaceae : palynology and systematics /". Pondichéry : [Paris] : Institut français ; [diff. J. Maisonneuve], 1985. http://catalogue.bnf.fr/ark:/12148/cb36651527x.

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Scotland, Robert Winning. "Palynology and systematics of Acanthaceae". Thesis, University of Reading, 1990. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.333341.

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Francis, Elizabeth. "The palynology of the Glencloy area". Thesis, Queen's University Belfast, 1987. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.317068.

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Al-Ghammari, Mutasam. "Ordovician-Silurian palynology of Oman. Vol.1". Thesis, University of Sheffield, 2010. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.531197.

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Warnes, Malcolm D. "The palynology of the Ohai coalfield, Southland". Thesis, University of Canterbury. Geology, 1988. http://hdl.handle.net/10092/10440.

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The Upper Cretaceous Morley Coal Measures in the Ohai Coalfield are one of three non-marine formations constituting the Ohai Group. In the past, seam correlation has generally been carried out using lithological criteria, however due to dramatic thinning and splitting of seams, associated faulting, and abrupt facies changes uncertainties in coal seam correlation have frequently arisen. In order to minimize lithostratigraphic uncertainties Couper (1964) pioneered a palynological zonation which demonstrated the potential of palynology for coal seam correlation. However, Couper's early work has proved unreliable and is in need of further refinement. Recent drillholes incorporating almost fully cored sequences of the Morley Formation have permitted further palynological examination of the coal measures. Nine drillholes were selected and 140 samples taken, at 10 metre intervals, for palynological analyses. The Morley Coal Measures are unconformably overlain by the Beaumont Coal Measures. This important boundary, though difficult to detect lithologically, is readily defined on palynological grounds. Biostratigraphic subdivision of the Morley Coal Measures was investigated by the application of three quantitative techniques. These entailed the construction and analysis of: (1) Standard pollen diagrams based on relative abundances of selected taxa and groups of taxa; (2) Pollen diagrams zoned by the numerical method of cluster analysis; (3) Ratios of selected taxa of recurrent and variably high frequency. Technique (1), involving relative abundance patterns of key taxa and groups of taxa was successful in providing a basis for subdivision of the Morley Coal Measures into three pollen zones, two interzonal units and two unzoned units. The three pollen zones were, in stratigraphically descending order: The Nothofagus kaitangata acme zone, the SPPA assemblage zone, and the Tricolpites reticulatus acme zone. Techniques (2) and (3) were, in all practicality, unproductive, although results suggested that, with refinement, cluster analysis could aid the zonation of pollen diagrams.
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Llewellyn, Rhian. "Palynology through the early Wenlock Ireviken Event". Thesis, University of Portsmouth, 2015. https://researchportal.port.ac.uk/portal/en/theses/palynology-through-the-early-wenlock-ireviken-event(e49e9e01-6288-4e69-8e6e-6de11ce90142).html.

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An early Sheinwoodian (Wenlock) chitinozoan assemblage is reported from a high-resolution investigation undertaken at Buttington Brick Pit, mid-Wales (positioned on the mid-shelf of the Welsh Basin in the early Wenlock). The lower Sheinwoodian strata from the locality are assigned herein to three local chitinozoan biozones: the margaritana chitinozoan Biozone, the bouniensis chitinozoan Biozone and the bella chitinozoan Biozone, which can all be correlated with the pre-established graptolite biostratigraphy of the section. The chitinozoan assemblage allows for, at least partial, stratigraphical correlation within the Welsh Basin and with other areas in Avalonia, Baltica, and peri-Gondwana. The ‘Interzone IV’ of Nestor (1994) is reported from the Welsh Basin for the first time. Chitinozoans are recovered throughout the section and show decreased diversity at levels within the riccartonensis graptolite Biozone. The lower part of the early Sheinwoodian positive carbon isotope excursion has been recognised previously from the section and a palaeoenvironmental investigation of the microphytoplankton assemblage herein has been undertaken from levels where carbon isotope data are available. The relative abundance of acritarchs (categorised by both genera and various informal morphotype groupings), prasinophytes, and sphaeromorphs within the microphytoplankton assemblage are considered to fluctuate with regard to proximity to shore, and are therefore considered diagnostic of sea-level change. The palaeoenvironmental signal from the microphytoplankton assemblage implies that a sea-level rise is associated with an interval of relatively low carbon isotope values that is superimposed upon the Sheinwoodian positive carbon isotope excursion, and recognised from multiple regions (e.g. Laurentia, Avelonia, and the Baltica).
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Dolez, Ludovic. "Évolution des paysages végétaux en Languedoc durant l’Holocène : apport de la palynologie à l’étude des milieux et des agrosystèmes". Thesis, Montpellier 3, 2018. http://www.theses.fr/2018MON30076/document.

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Cette thèse se propose d’étudier l’évolution des milieux et des agrosystèmes en Languedoc durant les derniers dix millénaires grâce à l’étude des paléo-végétations. Tout en réévaluant les recherches anciennes, ce travail affine la résolution temporelle des mutations paysagères enregistrées et apporte une vision à l’échelle du Languedoc occidental, par l’étude des bassins versants de l’Aude et de l’Hérault. À partir de l’analyse palynologique de carottages effectués dans des zones lagunaires proches d’Agde et de Narbonne, ce travail met en exergue la coévolution entre milieux et agrosystèmes, tant sur le temps long que sur le temps de l’Homme, en analysant les particularités et les rapprochements entre dynamiques de ces deux bassins versants comme les stratégies d’exploitation du territoire développées par l’Homme, l’utilisation de ressources végétales spécifiques ainsi que les types et zones de cultures et de pâturages, au niveau des aires littorales, mais aussi dans l’arrière-pays languedocien
This thesis studies the evolution of environments and agricultural systems in Languedoc during the last ten millennia through the paleo-vegetation. Reassessing old research, this work refines the temporal resolution of the landscape changes and provides vision at the western Languedoc scale, by the study of Aude and Hérault rivers watershed. From the pollen analyzes of cores drilled in lagoons close to Agde and Narbonne, this work highlights the coevolution between agricultural systems and environments, both long time and Man time, analyzing particularities and dynamic connections between these two watersheds like the territorial exploitation strategies developed by humans, the use of specific plant resources and the types and areas of crops and pastures, in coastal areas and in the Languedoc hinterland
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Watanasak, Manas. "Mid-tertiary palynology of onshore and offshore Thailand /". Title page, contents and abstract only, 1988. http://web4.library.adelaide.edu.au/theses/09PH/09phm267.pdf.

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Whelan, Gillian M. "The palynology of selected Ordovician localities in Scotland". Thesis, University of Glasgow, 1988. http://theses.gla.ac.uk/872/.

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Ordovician samples have been collected from various places from within three separate terranes in Scotland; the Highland Border Complex, the Southern Uplands and the Midland Valley. The samples have been palynologically processed and their assemblages studied with the aim of understanding some of the palaeoecological, biostratigraphical and thermal relationships of the three areas.Seventy one samples have been processed from nine localities of the Highland Border Complex and these have yielded fifteen species of chitinozoans in four genera, as well as indeterminate species of those genera. There are also five species of acritarchs in four genera as well as other microfossils. Black shales from the Complex yield the most diverse palynomorph assemblages, and were probably deposited from Arenig through to Caradoc although not necessarily at the same time in different parts of the basin. The preservation of palynomorphs appears to be better in the west of Scotland than in the east.From the Southern Uplands samples have been processed from Coldingham Bay and proved barren, from Barrhill the assemblages are poor, but from the Ordovician-Silurian bondary beds (C. peltifer to P. acuminatus Zones) at Dob's Linn they are quite diverse although abundance is very low, with forty three samples yielding thirty three species of acritarchs in eighteen genera, thirty one species of chitinozoans in thirteen genera and various other microfossils. The boundary cannot be delineated using the palynological assemblages, and although Tylotopalla sp. A and Ancyrochitina ancyrea Eisenack 1931 are common in most of the samples from the boundary the palynomorphs do not appear to mirror the changes that occur in the graptolite assemblages.From the Midland Valley samples have been processed from eight miscellaneous localities in the region of Girvan, giving very little biostratigraphical data, although one sample from Doularg Hill is dated as upper Arenig to lower Llanvirn. A section of twelve samples processed from the Mill and Shalloch Formations (D. complanatus and D. anceps Zones) at Woodland Point, Girvan, has yielded thirty five species of chitinozoans in twelve genera including a new species Angochitina woodlandensis and five new combinations; Belonechitina comma (Eisenack 1959), Belonechitina hirsuta (Laufeld 1967). Belonechitina micracantha (Eisenack 1931), Belonechitina schopfi subsp. americana (Taugourdeau 1965), and Belonechitina seriespinosa (Jenkins 1969). There are also forty seven species of acritarchs in twentyone genera, including two new species; Actinotodissus woodlandense, and Goniosphaeridium girvanense, and many scolecodonts. Spores are common and three species are recognised at Woodland Point. The samples are dated as Upper Ordovician and Calpichitina lenticularis (Bouche 1965) and Acanthochitina barbata appear to be important Upper Ordovician indicators, possibly being near-shore species as they are not found in rocks of the same age at Dob's Linn. Calpichitina lenticularis is very important in one sample and less so in all the others and it is suggested that it may be reworked. The palaeoecological picture at Woodland point shows an offshore situation in the Mill Formation, becoming more near-shore at the base of the Shalloch Formation and then more off-shore again.The palaeoecology of both Dob's Linn and Woodland Point are discussed and chitinozoans found to be more common in black shales than grey mudstones, although the acritarchs do not appear to be preferentially found in grey mudstones or black shales. Netromorph acritarchs are less common at Dob's Linn than was expected, but are very common at Woodland Point which may suggest that the sediments at Woodland Point were deposited more offshore than those at Dob's Linn but were more greatly influenced by turbiditic material. Sphaeromorph acritarchs at Woodland Point are very common and due to the variable thickness of the walls it is suggested that there is a mixing of near-shore and off-shore species, possibly by the turbiditic action mentioned above. Belonechitina is markedlymore important at Woodland Point than at Dob's Linn the reverse of which is true with Cyathochitina . The suggested reason for this is that Belonechitina is a near-shore species whilst Cyathochitina is an off-shore species. Veryhachium appears to become more important towards the end of the Ordovician, as a sample each from Woodland Point and Dob's Linn contain three species of this relatively rare genus, although the significance of this is not yet known.The sample from Dob's Linn and Woodland Point are compared with published works using the jacquard Coefficient and the results presented. The samples at Dob's Linn are compared with the Ordovician-Silurian boundary sediments elsewhere, and although different species are present at Dob's Linn and on Anticosti Island, and the abundance and diversity is lower at Dob's Linn, the boundary in Scotland has a much better palynomorph assemblage than was expected. The boundary assemblage presented here is quite similar to the one in Skane, Sweden.Finally the thermal history of the samples is discussed, and a general trend appears, with the samples from Girvan being the least altered, those from the Southern Uplands being moderately altered and finally the Highland Border Complex samples which have been subjected to temperatures probably between 200 and 300oC, and thus strongly altered.
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Gray, Catherine Elizabeth Darnell. "Characterising the Namaqualand Mudbelt: Chronology, Palynology and Palaeoenvironments". Doctoral thesis, University of Cape Town, 2009. http://hdl.handle.net/11427/4856.

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This multiproxy study explores the palaeoenvironmental record of two cores, H2 and H7, from the Namaqualand Mudbelt representing an arid and highly variable landscape. As bulk organic radiocarbon ages previously proved problematic, with anomalous reversals, the primary objective was to improve chronology and palaeoenvironmental reconstructions through high resolution 813C, 81SN and pollen analysis, with the aid of principal component analysis. Bulk organic radiocarbon dating of the surface sediment had previously yielded older than expected ages. New 210Pb analysis has established that these surface sediments are modem and radiocarbon ages are now recalibrated to yield an adjusted age of ±3 470 cal yr BP at the base of the more distal core, H7. Pollen spectra correlate well with stable isotopes and include recent disturbance indicators in the Succulent Karoo, Grassland, Karoo expansion, stock farming, impoundment, saltmarsh degradation and increase in domestic cereal cultivation. The proximal and distal mudbelt sites are, however, isotopically distinct, with 813C, inverse nitrogen and C/N ratios characterising H2 as more terrestrial. The excursion towards C3-rich values at around 6m depth in the proximal mudbelt suggests an increase in marine sources and C3 vegetation, while associated pollen aridity indicators implicate reduced inland flooding. This is contrasted against more humid conditions at 420 cm. Stronger upwelling occurred in near-surface distal mudbelt sediment and an influx of the Buffels River sediment flooded the region at ±3470 yr BP, indicating cooler, less arid conditions. 813C studies reveal the Lower Xobies palaeoflood deposit to be less C4-rich than expected, possibly due to sediment source, and is strikingly isotopically similar to the distal mudbelt. The palaeoenvironmental interpretation of the pollen assemblage, isotopes and chronology presents an improved understanding of the region represented in the mudbelt sediments. This corresponds well with established records of the last ±3 500 years and human induced land use change within the Orange River Catchment. Results also highlight the dynamics of the Orange River, which, combined with a highly variable climate, suggest that caution should be exercised to avoid over-interpreting the level at which environmental changes can meaningfully be reconstructed in arid landscapes, particularly those which are subject to sporadic and catastrophic flooding events.
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Libros sobre el tema "Palynology"

1

Thanikaimoni, G. Mangrove palynology. Pondicherry: UNDP/UNESCO Regional Project on Training and Research on Mangrove Ecosystems, RAS/79/002, 1987.

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Grey, Kathleen. Ediacaran palynology of Australia. Canberra: Association of Australasian Palaeontologists, 2005.

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3

J, Jansonius, McGregor D. C. 1929- y American Association of Stratigraphic Palynologists. Foundation., eds. Palynology: Principles and applications. [College Station, Tex.]: American Association of Stratigraphic Palynologists Foundation, 1996.

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Seetharam, Y. N. Clusiaceae: Palynology and systematics. Pondichéry, Inde: Institut français de Pondichéry, 1985.

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Erdtman, Gunnar. Erdtman's handbook of palynology. 2a ed. Copenhagen: Munksgaard, 1992.

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A, Jell P. y Association of Australasian Palaeontologists, eds. Studies in Australian Mesozoic palynology. Sydney: Association of Australasian Palaeontologists, 1987.

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Yoram, Eshet y Conway Brian H, eds. Paleozoic-mesozoic palynology of Israel. Jerusalem: Geological Survey of Israel, 1990.

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J, Batten D. y Keen Michael C, eds. Northwest European micropalaeontology and palynology. Chichester: E. Horwood for the British Micropalaeontological Society, 1989.

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W, Dimbleby G. The palynology of archaeological sites. London: Academic Press, 1985.

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Thomas, Barry. Bibliography of palaeobotany & palynology, 1990-1991. Cardif: Department of Botany, National Museum of Wales, 1992.

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Capítulos de libros sobre el tema "Palynology"

1

Pandey, Arun K. "Palynology". En Reproductive Biology of Angiosperms, 69–80. Boca Raton: CRC Press, 2022. http://dx.doi.org/10.1201/9781003260097-5.

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Adams-Groom, Beverley. "Forensic Palynology". En Forensic Ecology Handbook, 153–67. Chichester, UK: John Wiley & Sons, Ltd, 2012. http://dx.doi.org/10.1002/9781118374016.ch10.

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Traverse, Alfred. "Paleogene Palynology". En Paleopalynology, 391–426. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-5610-9_14.

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Traverse, Alfred. "Neogene Palynology". En Paleopalynology, 427–61. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-5610-9_15.

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Traverse, Alfred. "Holocene Palynology". En Paleopalynology, 463–95. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-5610-9_16.

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Traverse, Alfred. "Devonian Palynology". En Paleopalynology, 199–227. Dordrecht: Springer Netherlands, 2007. http://dx.doi.org/10.1007/978-1-4020-5610-9_8.

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Mendonça, Claudia Barbieri Ferreira, Leila Nunes Morgado, Gabriel Henrique Gomes de Souza Freitas Teixeira, Elen de Lima Aguiar-Menezes, Thiago Sampaio de Souza, Vinicius José Fernandes, Alice Teodorio Lixa, Roberto Lourenço Esteves y Vania Gonçalves-Esteves. "Ecological Palynology". En Aspects of Brazilian Floristic Diversity, 135–51. Cham: Springer International Publishing, 2022. http://dx.doi.org/10.1007/978-3-031-07453-0_6.

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Williams, Graham, Robert Fensome, Merrell Miller y Jonathan Bujak. "Microfossils: Palynology". En Selective Neck Dissection for Oral Cancer, 1–15. Cham: Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-02330-4_146-1.

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Laurence, Andrew R. y Vaughn M. Bryant. "Forensic Palynology". En Encyclopedia of Criminology and Criminal Justice, 1741–54. New York, NY: Springer New York, 2014. http://dx.doi.org/10.1007/978-1-4614-5690-2_169.

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Milne, Lynne A., Vaughn M. Bryant y Dallas C. Mildenhall. "Forensic Palynology". En Forensic Botany, 112–46. 2a ed. Boca Raton: CRC Press, 2024. http://dx.doi.org/10.4324/9780429272615-10.

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Actas de conferencias sobre el tema "Palynology"

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Borges, Felipe Silveira Brito, Juliana Velasques Balta, Milad Roghanian, Ariadne Barbosa Gonçalves, Marco Alvarez y Hemerson Pistori. "The interference of optical zoom in human and machine classification of pollen grain images". En Workshop de Visão Computacional. Sociedade Brasileira de Computação - SBC, 2021. http://dx.doi.org/10.5753/wvc.2021.18897.

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Palynology can be applied to different areas, such as archeology and allergy, where it is constantly growing. However, no publication comparing human classifications with machine learning classifications at different optical scales has been found in the literature. An image dataset with 17 pollen species that occur in Brazil was created, and machine learning algorithms were used for their automatic classification and subsequent comparison with humans. The experiments presented here show how machine and human classification behave according to different optical image scales. Satisfactory results were achieved, with 98.88% average accuracy for the machine and 45.72% for human classification. The results impact a single scale pattern for capturing pollen grain images for both future computer vision experiments and for a faster advance in palynology science.
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Hazel, Alexander M. "Identifying floral hosts of cerambycid beetles using palynology". En 2016 International Congress of Entomology. Entomological Society of America, 2016. http://dx.doi.org/10.1603/ice.2016.113858.

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Sapelko, T. V. y D. O. Sadokov. "PALYNOLOGY OF THE LAKES OF THE MOLOGA-SHEKSNA LOWLAND". En Актуальные проблемы современной палинологии. Москва: Общество с ограниченной ответственностью "Издательство ГЕОС", 2022. http://dx.doi.org/10.54896/9785891188532_2022_67.

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Mathewes, Rolf W. "FORENSIC PALYNOLOGY IN CANADA - FROM DELGAMUUKW TO HOMICIDE INVESTIGATION". En GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-306172.

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Bernhardt, Christopher, Diana Carriker, Jodi Webb, Libby Stern y Ian Saginor. "FINGERPRINT POWDER AS A SOURCE OF CONTAMINATION IN FORENSIC PALYNOLOGY". En Joint 72nd Annual Southeastern/ 58th Annual Northeastern Section Meeting - 2023. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023se-385784.

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Smith, Vann, Sophie Warny, Vivi Vajda, Johan Vellekoop, David M. Jarzen y Thomas D. Demchuk. "PALEOCENE-EOCENE TERRESTRIAL PALYNOLOGY OF THE CHICXULUB IMPACT CRATER, IODP 364". En GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-334630.

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Cabrera, Ryan J., Christopher A. Marsh, L. Olivia VanderEspt, Liberty F. Smallwood, Ingrid Romero, Noelia B. Nuñez Otaño, Diana Ochoa y Jennifer O'Keefe. "TROPICAL FUNGAL PALYNOLOGY OF EARLY-MIDDLE MIOCENE SEDIMENTS FROM NORTHWESTERN PERU". En Joint 72nd Annual Southeastern/ 58th Annual Northeastern Section Meeting - 2023. Geological Society of America, 2023. http://dx.doi.org/10.1130/abs/2023se-386101.

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Kondas, Marcelina. "THE PALYNOLOGY OF LOWER CARBONIFEROUS DEPOSITS OF THE HOLY CROSS MTS., POLAND". En GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-336377.

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Martínez, Erika Loyola, Enrique Martínez Hernández y José Rafael Barboza Gudiño. "Palynology Studies in Lower to Middle Jurassic Red Beds of Northeastern Mexico". En 2020 AAPG Hedberg Conference: Geology and Hydrocarbon Potential of the Circum-Gulf of Mexico Pre-Salt Section. Tulsa, OK, USA: American Association of Petroleum Geologists, 2020. http://dx.doi.org/10.1306/51654martinez2020.

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Cárdenas, Damián, Francisca E. Oboh-Ikuenobe, Francisca E. Oboh-Ikuenobe, Carlos Jaramillo y Carlos Jaramillo. "REDUCING THE LATITUDINAL BIAS IN NEOGENE MARINE PALYNOLOGY: INVESTIGATING THE NEOTROPICAL FOSSIL RECORD". En GSA Annual Meeting in Phoenix, Arizona, USA - 2019. Geological Society of America, 2019. http://dx.doi.org/10.1130/abs/2019am-333479.

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Informes sobre el tema "Palynology"

1

Waanders, Gerald. Palynology Evaluation Results From the Duchesne 30' x 60' Quadrangle, Duchesne and Wasatch Counties, Utah. Utah Geological Survey, mayo de 2023. http://dx.doi.org/10.34191/ofr-750.

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This Open-File Report makes available data from palynology evaluations completed to determine the age and depositional environment of rock samples collected during geologic investigations funded or partially supported by the Utah Geological Survey (UGS) and the U.S. Geological Survey National Cooperative Geologic Mapping Program (STATEMAP). Table 1 provides the sample numbers and locations for the palynology data. The reference listed in table 1 provides additional information such as sample location, geologic setting, and interpretation of the samples in the context of the area where they were collected.
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Ravn, R. L. Palynology photos from selected North Slope wells. Alaska Division of Geological & Geophysical Surveys, septiembre de 2016. http://dx.doi.org/10.14509/29677.

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Mudie, P. J. Palynology of the CESAR cores, Alpha Ridge. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1985. http://dx.doi.org/10.4095/120330.

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Zippi, P. A. Palynology of Tertiary Holitna outcrops, McGrath and Talkeetna quadrangles. Alaska Division of Geological & Geophysical Surveys, 2001. http://dx.doi.org/10.14509/2736.

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Dabros, M. J. y P. J. Mudie. An Automated Microscope System For Image Analysis in Palynology and Micropaleontology. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1986. http://dx.doi.org/10.4095/120356.

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Utting, J., J. D. Keppie y P. S. Giles. Palynology and stratigraphy of the lower carboniferous Horton Group, Nova Scotia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127720.

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Rouse, G. E., K. A. Lesack y J. M. White. Palynology of Cretaceous and Tertiary Strata of Georgia Basin, southwestern British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1990. http://dx.doi.org/10.4095/131445.

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8

Hotton, Carol L. y Zachary W. Anderson. Palynology Results for the Wanship 7.5' Quadrangle, Summit and Morgan Counties, Utah. Utah Geological Survey, septiembre de 2020. http://dx.doi.org/10.34191/ofr-726.

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9

McNeil, D. H., J. Dixon y K. M. Bell. The age, foraminifera, and palynology of the Upper Cretaceous Eagle Plain Group, northern Yukon. Natural Resources Canada/CMSS/Information Management, 2021. http://dx.doi.org/10.4095/328237.

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A re-evaluation of the age of the formations comprising the Eagle Plain Group of northern Yukon was necessitated by widely disparate age determinations in recent years from various authors. Maximum age estimates for the base of the group have varied from middle Albian to Cenomanian, and age estimates for the uppermost strata varied by an even greater range, from Cenomanian to late Maastrichtian. A re-examination of new and archival foraminiferal and palynological data indicates an age range of Cenomanian to late Maastrichtian for the Eagle Plain Group. The late Maastrichtian age is derived from palynology from the northeasternmost area of Eagle Plain. However, the stratigraphic relationship of these youngest beds within Eagle Plain Group remains uncertain. Marine strata of the Eagle Plain Group contain foraminiferal indices that correlate with long-established regional foraminiferal zones from the Mackenzie Delta area. The Cenomanian Zone of Trochammina superstes occurs in the Parkin and Boundary Creek formations of Eagle Plain and Mackenzie Delta, respectively. The Haplophragmoides bilobatus and overlying Glaphyrammina spirocompressa zones occur in the Burnthill Creek and Smoking Hills formations of Eagle Plain and Mackenzie Delta, respectively. Reworked microfossils are a conspicuous feature of strata within the Eagle Plain Group. The basal sandstone of the Parkin Formation, for example, contains an assemblage of foraminifera that is entirely reworked. Palynomorph assemblages through the Eagle Plain Group have been estimated at as much as 99% reworked in some strata.
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10

Waanders, Gerald L. Palynology Evaluation Results from the Provo, Duchesne, and Rush Valley 30' x 60' Quadrangles, Utah. Utah Geological Survey, julio de 2020. http://dx.doi.org/10.34191/ofr-720.

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