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Journal articles on the topic 'Thanatocenosis'

Author: Grafiati

Published: 5 June 2025

Last updated: 2 August 2025

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1

Sokolova, E. A. "CLIMATIC FLUCTUATIONS IN THE MIDDLE LATITUDES OF THE NORTHERN HEMISPHERE ACCORDING TO THE STUDY OF CAMPANIAN PLANKTONIC FORAMINIFERA." Journal of Oceanological Research 49, no. 2 (2021): 80–99. http://dx.doi.org/10.29006/1564-2291.jor-2021.49(2).6.

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To reconstruct the climatic fluctuations that occurred in the middle latitudes of the Northern Hemisphere in the Atlantic Ocean in the Campanian Age, the systematic composition of the shells of planktonic foraminifera was studied from core samples from seven deep-water drilling holes. The identified foraminiferal assemblages are assigned to two types (boreal and intermediate) and one subtype (warm boreal) thanatocenosis. On the basis of their spatial distribution, the position of climatic zones for sections of the early, middle, beginning and end of the late Campanian was determined. Different

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2

Alexandrowicz, Stefan Witold. "A mollusc thanatocenosis in the Nile River Valley near Wadi Halfa (N Sudan)." Folia Malacologica 9, no. 1 (2009): 39–43. http://dx.doi.org/10.12657/folmal.009.005.

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3

Yushin, K. I., and V. N. Komarov. "About a new type of redeposition of fossils." Proceedings of higher educational establishments. Geology and Exploration, no. 3 (June 28, 2017): 52–55. http://dx.doi.org/10.32454/0016-7762-2017-3-52-55.

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At the final stage of the taphonomic cycle, after the deposit has gone to the surface in a result of different processes, the alteration of the deposit in the zone of surface weathering occurs, due to the mechanic destruction as well as the processes of soiution and replacement. A phenomenon of the deposition in thanatocenosis the reburied fossils - redeposition - has a widespread occurrence in this time. On the basis of the unique finding of the cervical vertebra of the Upper Pleistocene European roe deer in the modern freshwater catfish (Silurus glanis Linnaeus) a new type of the fossils red

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4

Lutaenko, Konstantin A. "Shell destruction of the bivalve mollusk Glycymeris yessoensis on a beach in Possjet Bay (the Sea of Japan)." Бюллетень Дальневосточного малакологического общества 24, no. 1/2 (2020): 82–95. http://dx.doi.org/10.24866/1560-8425/2020-24/82-95.

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На пляже м. Шелеха (зал. Посьета) изучали распределение пустых раковин, створок и фрагментов двустворчатого моллюска Glycymeris yessoensis (Sowerby III, 1889). Всего было взято 13 проб с площади 1 м², плотность раковинного материала варьировала от 4 до 44 экз./м². Доля целых раковин от общего числа экземпляров на всем пляже невелика – 14%, т.к. раковины этого вида легко дисартикулируются при высыхании лигамента. Однако удельный вес экземпляров (от общего числа обнаруженных во всех пробах раковин и створок) с механическими повреждениями (12%) и со следами сохранившегося периостракума (31%) указ

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5

Tarruella, Ruestes Antoni, and Joaquin Lopez-Soriano. "Moluscos marinos del Baix Camp (Tarragona, NE Península Ibérica)." Spira 2, no. 1 (2006): 1–16. https://doi.org/10.5281/zenodo.8275899.

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Marine mollusks from Baix Camp (Tarragona, NE Iberian Peninsula). In this paper, species from beach thanatocenoses of Baix Camp area (localities of Montroig, L’Hospitalet de l’Infant and Vandellòs) in the province of Tarragona are reported, with a total of 477 collected species. This is an area of high malacological diversity; it is noteworthy the presence of at least three species never described before for the Catalan and/or Iberian malacofauna: Monoptygma modesta, Cerithium cf. protractum and Cerithium cf. haustellum.

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6

Deiana, Giacomo, Luciano Lecca, Rita Melis, Mauro Soldati, Valentino Demurtas, and Paolo Orrù. "Submarine Geomorphology of the Southwestern Sardinian Continental Shelf (Mediterranean Sea): Insights into the Last Glacial Maximum Sea-Level Changes and Related Environments." Water 13, no. 2 (2021): 155. http://dx.doi.org/10.3390/w13020155.

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During the lowstand sea-level phase of the Last Glacial Maximum (LGM), a large part of the current Mediterranean continental shelf emerged. Erosional and depositional processes shaped the coastal strips, while inland areas were affected by aeolian and fluvial processes. Evidence of both the lowstand phase and the subsequent phases of eustatic sea level rise can be observed on the continental shelf of Sardinia (Italy), including submerged palaeo-shorelines and landforms, and indicators of relict coastal palaeo-environments. This paper shows the results of a high-resolution survey on the contine

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7

Deiana, Giacomo, Luciano Lecca, Rita Teresa Melis, Mauro Soldati, Valentino Demurtas, and Paolo Emanuele Orrù. "Submarine Geomorphology of the Southwestern Sardinian Continental Shelf (Mediterranean Sea): Insights into the Last Glacial Maximum Sea-Level Changes and Related Environments." Water 13, no. 2 (2021): 155. http://dx.doi.org/10.3390/w13020155.

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During the lowstand sea-level phase of the Last Glacial Maximum (LGM), a large part of the current Mediterranean continental shelf emerged. Erosional and depositional processes shaped the coastal strips, while inland areas were affected by aeolian and fluvial processes. Evidence of both the lowstand phase and the subsequent phases of eustatic sea level rise can be observed on the continental shelf of Sardinia (Italy), including submerged palaeo-shorelines and landforms, and indicators of relict coastal palaeo-environments. This paper shows the results of a high-resolution survey on the contine

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8

Hoffman, Leon, Serge Gofas, and André Freiwald. "A large biodiversity of "skeneimorph" (Gastropoda: Vetigastropoda) species from the South Azorean Seamount Chain, with the description of seventeen new species." Iberus supplement 9 [to vol. 38] (December 10, 2020): 1–82. https://doi.org/10.5281/zenodo.4969080.

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Forty-six “skeneimorph” species from the South Azorean Seamount Chain (SASC) have been studied. These comprise taxa in the superfamilies Trochoidea (family Skeneidae) and Seguenzioidea (families Trochaclididae, Pendromidae, Eudaroniidae and several genera which are not assigned to a family). Seventeen new species are proposed, fifteen in Seguenzioidea (<em>Trochaclis fortis </em>n. sp., <em>Trochaclis carinata </em>n. sp., <em>Trochaclis platoensis </em>n. sp., <em>Adeuomphalus axistriatus </em>n. sp., <em>Adeuomphalus curvistriatus </em>n. sp., <em>Eudaronia spirata </em>n. sp., <

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9

Rogozin, A. G., N. A. Isakova, and L. V. Snit’ko. "Retrospective of diatom diversity dynamics in thanatocenoses under climate change." Inland Water Biology 10, no. 2 (2017): 153–57. http://dx.doi.org/10.1134/s1995082917020122.

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10

Avila-Serrano, G. "Taphonomic processes in recent thanatocenoses at playa el pelícano, baja california." Ciencias Marinas 26, no. 4 (2000): 677–94. http://dx.doi.org/10.7773/cm.v26i4.604.

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11

Alexandrowicz, Stefan Witold. "Mollusc thanatocenoses in the lower course of the Osam River (Northern Bulgaria)." Folia Malacologica 7, no. 2 (2009): 177–82. http://dx.doi.org/10.12657/folmal.007.017.

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12

Saidova, Kh M., and E. A. Sokolova. "PALEOBIOGEOGRAPHICAL RECONSTRUCTIONS FOR THE END OF THE LATE CAMPANIANS BY PLANKTONIC FORAMINIFERA IN THE PACIFIC OCEAN." Journal of Oceanological Research 51, no. 2 (2023): 48–69. http://dx.doi.org/10.29006/1564-2291.jor-2023.51(2).4.

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The paper considers the results of the analysis of the taxonomic composition of planktonic foraminifera (PF) from the end of the Late Campanian in the Pacific Ocean. To identify the latitudinal-zonal faunas of the PF, an assessment was made of the species similarity and differences of the PF complexes of the same age from different wells. Based on the difference in species composition, the fauna of the PF is divided into non-arctic regional and oceanic latitudinal-zonal: subtropical western, tropical central and subtropical central oceanic faunas. To reconstruct the climatic fluctuations that

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13

Yanygina, L. V., and D. D. Volgina. "Age and size characteristics of alien mollusks Viviparus viviparus L. in the coastal thanatocoenosis of Novosibirsk reservoir." Ukrainian Journal of Ecology 9, no. 3 (2019): 412–14. http://dx.doi.org/10.15421/2019_118.

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Viviparus viviparus L. is the most numerous alien species of the Novosibirsk reservoir. In some parts of the reservoir V. viviparus creates settlements with a very high density. After the death of mollusks in the bottom sediments and on the banks of the reservoir, large areas of accumulation of empty shells are formed. Due to their strong structure, the shells are poorly decomposed and can serve as a generalized indicator of the state of the mollusk population over a long time. We analyzed the size and age characteristics of the V. viviparus shells in thanatocenoses of the Novosibirsk reservoi

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14

Alexandrowicz, Stefan Witold. "Mollusc thanatocenoses of the Vistula River in the southern part of the Cracow Upland." Folia Malacologica 8, no. 3 (2009): 171–79. http://dx.doi.org/10.12657/folmal.008.012.

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15

Michel, RAKOTONIMANANA Rivoniaina. "Paléoécologie Et Taphonomie Du Crétacé Moyen d’Ambatolafia Bassin De Mahajanga." International Journal of Progressive Sciences and Technologies 39, no. 1 (2023): 116. http://dx.doi.org/10.52155/ijpsat.v39.1.5359.

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Une analyse taphonomique réalisée sur le site de l'Albien inférieur de la section des carrières d’Ambatolafia permet de retracer la genèse et la paléoécologie de cette localité. Il est trouvé à Ambatolafia un mélange de deux types de gisement thanatocenose et paléobiocenose respectivement par des organismes allochtones(Ammonites, Bélemnites) et par des organismes autochtones (Fossarus, Gyrodes, Venelicardia,Arca), Ambatolafia est une formation paratochtone. Du point de vue paléoenvironnementale, l’Albien d’Ambatolafia constitue un milieu exclusivement marin (mer confinée), à profondeur moyenne

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16

Sitzia, Luca. "Etude préliminaire du remplissage sédimentaire de l'Igue du Gral et implications pour l'accumulation des restes fauniques." Revue de Paléobiologie 43, no. 2 (2024): 87–105. https://doi.org/10.5281/zenodo.13860454.

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Preliminary study of the sedimentary filling of the Igue du Gral and its implications for the accumulation of faunal remains.- Bone caves such as sinkholes constitute remarkable sources of information for researchers interested in the paleoecology of fossil faunas. Moreover, these accumulations contain assemblages not or little affected by human intervention and can, therefore, serve as a source of comparison and contrast with contemporaneous assemblages from archaeological sites. In both cases, understanding the geomorphological context and the sedimentary dynamics remains fundamental when pr

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17

Yassini, I., and BG Jones. "Ostracoda in Lake Illawarra: Environmental factors, assemblages and systematics." Marine and Freshwater Research 38, no. 6 (1987): 795. http://dx.doi.org/10.1071/mf9870795.

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Major controls of the distribution pattern and abundance of living ostracod populations in Lake Illawarra, a coastal lagoon south of Wollongong, New South Wales, are salinity and the benthic flora. The biocenotic ostracod assemblage from the intertidal zone around Windang Island is a typical, diverse, upper sublittoral, open ocean fauna. The lake entrance channel, which is a transport corridor for marine sediments into the lagoon, has a restricted ostracod biocenose (14 species) but contains an additional 72 species in the diverse thanatocenose resulting from the mixing of estuarine and marine

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18

Kovanda, Jiří, Ivan Horáček, and Radka Symonová. "Pátek, Levousy a Chlumčany – významné fosiliferní středopleistocénní lokality na pravém břehu Ohře mezi Louny a Libochovicemi [Pátek, Levousy and Chlumčany – important mid-pleistocene localities on the right bank of the Ohře River between Louny and Libochovice]." Malacologica Bohemoslovaca 3 (July 26, 2005): 149–72. http://dx.doi.org/10.5817/mab2002-3-149.

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Due to a complete predominance of non-calcareous fluvial sediments in the Czech Republic, any find of fossil malacofauna is always considered as rare. The present work describes three localities in the Ohře river area, which contain, especially in the case of the Pátek locality, very abundant mid-Pleistocene malacofaunas. They were mainly collected in the floodplain fine-grained loam and back swamp deposits but also in sandy gravels. The molluscan thanatocenoses from localities near the Pátek village indicate the interglacial maximum (with up to 25 forest species s.l.), which developed directl

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19

Kovanda, Jiří, Ivan Horáček, and Radka Symonová. "Pátek, Levousy a Chlumčany – významné fosiliferní středopleistocénní lokality na pravém břehu Ohře mezi Louny a Libochovicemi [Pátek, Levousy and Chlumčany – important mid-pleistocene localities on the right bank of the Ohře River between Louny and Libochovice]." Malacologica Bohemoslovaca 3 (July 26, 2005): 149–72. http://dx.doi.org/10.5817/mab2005-3-149.

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Due to a complete predominance of non-calcareous fluvial sediments in the Czech Republic, any find of fossil malacofauna is always considered as rare. The present work describes three localities in the Ohře river area, which contain, especially in the case of the Pátek locality, very abundant mid-Pleistocene malacofaunas. They were mainly collected in the floodplain fine-grained loam and back swamp deposits but also in sandy gravels. The molluscan thanatocenoses from localities near the Pátek village indicate the interglacial maximum (with up to 25 forest species s.l.), which developed directl

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20

Kovanda, Jiří, Ivan Horáček, and Radka Symonová. "Pátek, Levousy a Chlumčany – významné fosiliferní středopleistocénní lokality na pravém břehu Ohře mezi Louny a Libochovicemi [Pátek, Levousy and Chlumčany – important mid-pleistocene localities on the right bank of the Ohře River between Louny and Libochovice]." Malacologica Bohemoslovaca 3 (May 4, 2005): 149–72. https://doi.org/10.5281/zenodo.3959776.

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Due to a complete predominance of non-calcareous fluvial sediments in the Czech Republic, any find of fossil malacofauna is always considered as rare. The present work describes three localities in the Ohře river area, which contain, especially in the case of the Pátek locality, very abundant mid-Pleistocene malacofaunas. They were mainly collected in the floodplain fine-grained loam and back swamp deposits but also in sandy gravels. The molluscan thanatocenoses from localities near the Pátek village indicate the interglacial maximum (with up to 25 forest species s.l.), which dev

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21

Калмыков, Н. П. "УСЛОВИЯ ФОРМИРОВАНИЯ ОРИКТОЦЕНОЗА ПЛИОЦЕНОВЫ Х М ЛЕКОПИТАЮ Щ ИХ (ХАМ БИНСКИЙ ХРЕБЕТ, Ю Г ВОСТОЧНОЙ СИБИРИ) ©". Грозненский естественнонаучный бюллетень 5, № 4(22) (2021). https://doi.org/10.25744/genb.2020.22.4.002.

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Дается общая картина геологической обстановки Западного Забайкалья с мезозоя до четвертичного периода, способствовавшая формированию предгорного шлейфа у подножия Хамбинского хребта. Приводится литология и минералогия аллювиальных и красноцветных отложений с фоссилиями рыб (Esox, Silurus) и млекопитающих (Primates, Lagomorpha, Rodentia, Carnivora, Proboscidea, Hyracoidea, Perissodactyla, Artiodactyla). Анатомическое сочленение костей, не разложившиеся копролиты, опавшие рога оленей указывают на автохтонность ориктоценоза, несколько смещенного относительно танатоценоза. Ограниченное время обита

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22

Schifino Valente, Ana Luisa. "South American Sea Lion Thanatocenotic Elements of in Sediments: Would be an Important Source of Environmental Contamination by Parasite Eggs?" Journal of Dairy & Veterinary Sciences 5, no. 2 (2018). http://dx.doi.org/10.19080/jdvs.2018.05.555657.

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