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1

Bracchi, Valentina Alice, Agostino Niyonkuru Meroni, Vivien Epis, and Daniela Basso. "Mollusk Thanatocoenoses Unravel the Diversity of Heterogeneous Rhodolith Beds (Italy, Tyrrhenian Sea)." Diversity 15, no. 4 (2023): 526. http://dx.doi.org/10.3390/d15040526.

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Emerging evidence of rhodolith bed complexity and heterogeneity poses a challenge to monitoring strategies and questions about the role of abiotic factors in controlling the observed morphostructural diversity. Mollusk thanatocoenoses quickly respond to environmental conditions, expressing fidelity to biocoenosis and representing, thus, a useful ecological/paleoecological tool to unravel this heterogeneity. In this research, we studied three distinct rhodolith beds from the Tyrrhenian Sea (Italy), in a range between 40 and 100 m of water depth, together with their mollusk thanatocoenoses, sedi
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2

Heinrich, Dirk. "Some remarks on the tem "Thanatocoenosis" especially "Anthropogenic Thanatocoenosis", with particular reference to fish remains." Archaeofauna, no. 3 (October 22, 1994): 93–97. https://doi.org/10.15366/archaeofauna1994.3.007.

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En el trabajo se lleva a cabo un repaso crítico a la compleja nomenclatura tafonómica valorando las características y razones de ser de algunos términos con vistas a diferenciarlos de otros similares. Asimismo se realiza una somera valoración del tipo de asociaciones de fauna susceptibles de proporcionar restos de peces.
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3

Utrilla, Olga, Serge Gofas, Javier Urra, et al. "Molluscs from benthic habitats of the Gazul mud volcano (Gulf of Cádiz)." Scientia Marina 84, no. 3 (2020): 273. http://dx.doi.org/10.3989/scimar.05027.17a.

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Molluscs from the Gazul mud volcano and its adjacent areas in the northern Gulf of Cádiz were studied using differ­ent sampling methods. This mud volcano has vulnerable deep-sea habitats and a potential high biodiversity. A total of 232 species were identified from the taxocoenosis and thanatocoenosis, of which 86 are new records for the Spanish margin of the Gulf of Cádiz, three of them are new records for Spanish waters and two species are new to science. The high species richness observed could be related to the combination of different sampling methods, the study of the thanatocoenosis, th
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4

Postawa, Tomasz. "Changes in bat fauna during the Middle and Late Holocene as exemplified by thanatocoenoses dated with 14C AMS from Kraków-Cz"stochowa Upland caves, Poland." Acta Chiropterologica 6, no. 2 (2004): 269–92. https://doi.org/10.5281/zenodo.13518754.

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(Uploaded by Plazi for the Bat Literature Project) Fossil material from 12 caves situated in the Kraków-Cz"stochowa Upland (southern Poland) was studied. In 17 samples of osteological material, 8,275 individuals (Minimal Number of Individuals, MNI = 4,571) of 12 bat species were identified. Thirteen separate thanatocoenoses were found (R × C test) from which bone material was dated using the 14C AMS method; 13 dates from 6,725 to 820 14C yr BP (yr BP) were obtained. Correspondence analysis for thanatocoenoses from the Atlantic and Subboreal periods distinguished two bat species groups and two
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5

Postawa, Tomasz. "Changes in bat fauna during the Middle and Late Holocene as exemplified by thanatocoenoses dated with 14C AMS from Kraków-Cz"stochowa Upland caves, Poland." Acta Chiropterologica 6, no. 2 (2004): 269–92. https://doi.org/10.5281/zenodo.13518754.

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(Uploaded by Plazi for the Bat Literature Project) Fossil material from 12 caves situated in the Kraków-Cz"stochowa Upland (southern Poland) was studied. In 17 samples of osteological material, 8,275 individuals (Minimal Number of Individuals, MNI = 4,571) of 12 bat species were identified. Thirteen separate thanatocoenoses were found (R × C test) from which bone material was dated using the 14C AMS method; 13 dates from 6,725 to 820 14C yr BP (yr BP) were obtained. Correspondence analysis for thanatocoenoses from the Atlantic and Subboreal periods distinguished two bat species groups and two
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6

Postawa, Tomasz. "Changes in bat fauna during the Middle and Late Holocene as exemplified by thanatocoenoses dated with 14C AMS from Kraków-Cz"stochowa Upland caves, Poland." Acta Chiropterologica 6, no. 2 (2004): 269–92. https://doi.org/10.5281/zenodo.13518754.

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(Uploaded by Plazi for the Bat Literature Project) Fossil material from 12 caves situated in the Kraków-Cz"stochowa Upland (southern Poland) was studied. In 17 samples of osteological material, 8,275 individuals (Minimal Number of Individuals, MNI = 4,571) of 12 bat species were identified. Thirteen separate thanatocoenoses were found (R × C test) from which bone material was dated using the 14C AMS method; 13 dates from 6,725 to 820 14C yr BP (yr BP) were obtained. Correspondence analysis for thanatocoenoses from the Atlantic and Subboreal periods distinguished two bat species groups and two
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7

Postawa, Tomasz. "Changes in bat fauna during the Middle and Late Holocene as exemplified by thanatocoenoses dated with 14C AMS from Kraków-Cz"stochowa Upland caves, Poland." Acta Chiropterologica 6, no. 2 (2004): 269–92. https://doi.org/10.5281/zenodo.13518754.

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(Uploaded by Plazi for the Bat Literature Project) Fossil material from 12 caves situated in the Kraków-Cz"stochowa Upland (southern Poland) was studied. In 17 samples of osteological material, 8,275 individuals (Minimal Number of Individuals, MNI = 4,571) of 12 bat species were identified. Thirteen separate thanatocoenoses were found (R × C test) from which bone material was dated using the 14C AMS method; 13 dates from 6,725 to 820 14C yr BP (yr BP) were obtained. Correspondence analysis for thanatocoenoses from the Atlantic and Subboreal periods distinguished two bat species groups and two
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8

Bernardez, P., M. Varela, Y. Pazos, R. Prego, and G. Frances. "Biocoenosis and thanatocoenosis of diatoms in a western Galician ria." Journal of Plankton Research 32, no. 6 (2010): 857–83. http://dx.doi.org/10.1093/plankt/fbq025.

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9

Ruggiero, Emma Taddei, Giuseppe Buono, and Pasquale Raia. "Bioerosion on Brachiopod Shells of a Thanatocoenosis of Alboràn Sea (Spain)." Ichnos 13, no. 3 (2006): 175–84. http://dx.doi.org/10.1080/10420940600853855.

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10

Cheli, Alessandro, Arianna Mancuso, Michele Azzarone, et al. "Climate variation during the Holocene influenced the skeletal properties of Chamelea gallina shells in the North Adriatic Sea (Italy)." PLOS ONE 16, no. 3 (2021): e0247590. http://dx.doi.org/10.1371/journal.pone.0247590.

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Understanding how marine taxa will respond to near-future climate changes is one of the main challenges for management of coastal ecosystem services. Ecological studies that investigate relationships between the environment and shell properties of commercially important marine species are commonly restricted to latitudinal gradients or small-scale laboratory experiments. This paper aimed to explore the variations in shell features and growth of the edible bivalve Chamelea gallina from the Holocene sedimentary succession to present-day thanatocoenosis of the Po Plain-Adriatic Sea system (Italy)
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11

NESTEROVICH, ANNA, and BETH E. CAISSIE. "Taxonomy and ultrastructure of Sinerima, a new genus of diatoms (Bacillariophyta), with a description of a new species, S. marigela." Phytotaxa 351, no. 3 (2018): 197. http://dx.doi.org/10.11646/phytotaxa.351.3.1.

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Based on light, scanning and transmission electron microscopy observations, a detailed description of a new marine fultoportulate diatom Sinerima marigela gen. et sp. nov. is presented. This new taxa is rare (<3% of the thanatocoenosis) in surface sediments in the Bering and Chukchi seas, but appears to have an association with high spring sea ice concentrations. The new monotypic genus is distinct due to its 1) lack of rimoportulae, 2) one-layer valves with marginal pseudoloculi, 3) characteristic velum composed of a cluster of short tubes, and 4) central part without either central fultop
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12

Costa, Gabriele, Giorgio Bavestrello, Simonepietro Canese, et al. "Sponges associated with stylasterid thanatocoenosis (Cnidaria, Hydrozoa) from the deep Ross Sea (Southern Ocean)." Polar Biology 45, no. 4 (2022): 703–18. http://dx.doi.org/10.1007/s00300-022-03023-6.

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13

Bonomo, S., A. Cascella, I. Alberico, et al. "Living and thanatocoenosis coccolithophore communities in a neritic area of the central Tyrrhenian Sea." Marine Micropaleontology 142 (June 2018): 67–91. http://dx.doi.org/10.1016/j.marmicro.2018.06.003.

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14

Albrecht, C., H. Vogel, T. Hauffe, and T. Wilke. "Sediment core fossils in ancient Lake Ohrid: testing for faunal change in molluscs since the Last Interglacial period." Biogeosciences Discussions 7, no. 3 (2010): 3969–99. http://dx.doi.org/10.5194/bgd-7-3969-2010.

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Abstract. Ancient Lake Ohrid is probably of early Pleistocene or Pliocene origin and amongst the few lakes in the world harboring an outstanding degree of endemic biodiversity. Although there is a long history of evolutionary research in Lake Ohrid, particularly on molluscs, a mollusc fossil record has been missing up to date. For the first time, gastropod and bivalve fossils are reported from the basal, calcareous part of a 2.6 m long sediment succession (core Co1200) from the north-eastern part of Lake Ohrid. Electron spin resonance (ESR) dating of mollusc shells from the same stratigraphic
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15

Albrecht, C., H. Vogel, T. Hauffe, and T. Wilke. "Sediment core fossils in ancient Lake Ohrid: testing for faunal change since the Last Interglacial." Biogeosciences 7, no. 11 (2010): 3435–46. http://dx.doi.org/10.5194/bg-7-3435-2010.

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Abstract. Ancient Lake Ohrid is probably of early Pleistocene or Pliocene origin and amongst the few lakes in the world harbouring an outstanding degree of endemic biodiversity. Although there is a long history of evolutionary research in Lake Ohrid, particularly on molluscs, a mollusc fossil record has been missing up to date. For the first time, gastropod and bivalve fossils are reported from the basal, calcareous part of a 2.6 m long sediment succession (core Co1200) from the north-eastern part of Lake Ohrid. Electron spin resonance (ESR) dating of mollusc shells from the same stratigraphic
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16

Šribar, Luka, and Jernej Pavšič. "Comparison of Biocoenosis with Thanatocoenosis from Adriatic, between the peninsula Istria and the river Po." Geologija 36, no. 1 (1994): 119–56. http://dx.doi.org/10.5474/geologija.1994.006.

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17

Zhivoglyadova, L. A., D. A. Vekhov, N. S. Elfimova, and N. K. Revkov. "Invasion of the alien clam Corbicula fluminea (O.F. Müller, 1774) in the irrigation canal system of the Lower Don Basin." Водные биоресурсы и среда обитания 8, no. 2 (2025): 7–18. https://doi.org/10.47921/2619-1024_2025_8_2_7.

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Background. The Asian clam Corbicula fluminea (O.F. Müller, 1774) is classified among the most dangerous invasive species in Europe and Russia. In 2017, C. fluminea was discovered in the Lower Don Вasin for the first time. At present, the expansion of the Asian clam in the Lower Don Basin is still ongoing. This conclusion is based on the discovery of a thanatocoenosis of C. fluminea in the Lower- Manych Irrigation System. Relevance. Investigation of the temporary communities of C. fluminea in the irrigation canals will make it possible to assess the role of artificial water bodies in the furth
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18

Snyder, Keith, Matthew McLain, Jared Wood, and Arthur Chadwick. "Over 13,000 elements from a single bonebed help elucidate disarticulation and transport of an Edmontosaurus thanatocoenosis." PLOS ONE 15, no. 5 (2020): e0233182. http://dx.doi.org/10.1371/journal.pone.0233182.

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19

Westman, P., and G. Sohlenius. "Variability in diatom thanatocoenosis in Holocene sediments of the northwestern Baltic Sea, Sweden ‐ a multicore approach." GFF 118, sup004 (1996): 72. http://dx.doi.org/10.1080/11035899609546364.

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20

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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21

Cruz-Pérez, Josseline Michelle, Ángel Raúl Herrera-Gutiérrez, Catalina Inés Cortés-Vélez, Rigoberto Guardado-France, Ismael Yarbuh, and Miguel A. Santa Rosa-del Río. "Structure, composition, and distribution of subtidal benthic foraminifera thanatocoenosis, San Luis Gonzaga Bay, northwestern Gulf of California, Mexico." Journal of South American Earth Sciences 110 (October 2021): 103411. http://dx.doi.org/10.1016/j.jsames.2021.103411.

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22

Shemesh, A., L. H. Burckle, and P. N. Froelich. "Dissolution and Preservation of Antarctic Diatoms and the Effect on Sediment Thanatocoenoses." Quaternary Research 31, no. 2 (1989): 288–308. http://dx.doi.org/10.1016/0033-5894(89)90010-0.

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AbstractComparison of Southern Ocean diatom populations from (i) surface ocean production, (ii) underlying Antarctic sediments, and (iii) laboratory dissolution experiments demonstrates that dissolution can account for the temporal and spatial variations in sedimentary diatom assemblages observed in Southern Ocean sediments. Increasing dissolution causes relative depletions in N. kerguelensis (K), enrichments in T. lentiginosa (L), and slight enrichments in E. antarctica (A). This reflects the relative susceptibility to dissolution of the three species that dominate Antarctic sediments. We hav
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23

Wattinne, Aurélia, Emmanuelle Vennin, and Patrick De Wever. "Evolution of carbonated, lacustrine environment, with stromatolites : a paleoecological approach (quarry of Montaigu-le-Blin, Limagne graben, Allier, France)." Bulletin de la Société Géologique de France 174, no. 3 (2003): 243–60. http://dx.doi.org/10.2113/174.3.243.

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Abstract The Aquitanian deposits of the quarry of Montaigu-le-Blin, located in the ≪ Limagne bourbonnaise », are characterized by lacustrine marl and limestone alternations. They display well-developed vegetal and fauna associations. The sedimentary deposits show an environment which allowed settlement of fresh water fauna. The deposits reveal variations of the water level and consequently of the water chemistry. These variations are characterized by alternations of anoxic and oxidizing lacustrine environments, which are due to periodic climatic changes (alternating more or less humid periods)
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24

Calcinai, Barbara, Teo Marrocco, Camilla Roveta, et al. "Porifera Associated with Deep-Water Stylasterids (Cnidaria, Hydrozoa): New Species and Records from the Ross Sea (Antarctica)." Journal of Marine Science and Engineering 12, no. 12 (2024): 2317. https://doi.org/10.3390/jmse12122317.

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Stylasterid corals are known to be fundamental habitat-formers in both deep and shallow waters. Their tridimensional structure enhances habitat complexity by creating refuges for a variety of organisms and by acting as basibionts for many other invertebrates, including sponges. Porifera represent crucial components of marine benthic assemblages and, in Antarctica, they often dominate benthic communities. Here, we explore the sponge community associated with thanatocoenosis, mostly composed of dead stylasterid skeletons, collected along the Western and Northern edges of the Ross Sea continental
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25

Lyson, Tyler R., and Walter G. Joyce. "A revision of Plesiobaena (Testudines: Baenidae) and an assessment of baenid ecology across the K/T boundary." Journal of Paleontology 83, no. 6 (2009): 833–53. http://dx.doi.org/10.1666/09-035.1.

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Over the course of the last two decades, the baenid taxon Plesiobaena has typically been thought to consist of two named species, Plesiobaena antiqua (Campanian) and Plesiobaena putorius (Paleocene), along with an unnamed species from the Maastrichtian, but the interrelationship of these three taxa was never explored in an explicit phylogenetic context. Herein we present or re-describe a number of relevant specimens and provide a cladistic analysis of Baenidae using species only as terminal taxa. The phylogenetic analysis clearly reveals that Plesiobaena in the traditional sense is a paraphyle
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26

Yassini, I., BG Jones, RJ King, M. Ayress, and KT Dewi. "Ostracod fauna associated with sublittoral kelp forest vegetation at Windang Island, New South Wales, Australia." Marine and Freshwater Research 46, no. 8 (1995): 1181. http://dx.doi.org/10.1071/mf9951181.

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Sublittoral kelp forests, such as those occupying the wave-dominated shallow marine rocky substrata around Windang Island, New South Wales, provide an important habitat for ostracods. This is reflected in the diverse biocoenotic assemblage (69 species, including one new genus and three new species) and populations of juveniles recorded from this area. The thanatocoenotic assemblage contributes a further 37 ostracod species. The total assemblage is more diverse than, and has only 17 species in common with, the previously documented intertidal biocoenotic assemblages around Windang Island. The d
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27

Romero, O., and D. Hebbeln. "Biogenic silica and diatom thanatocoenosis in surface sediments below the Peru–Chile Current: controlling mechanisms and relationship with productivity of surface waters." Marine Micropaleontology 48, no. 1-2 (2003): 71–90. http://dx.doi.org/10.1016/s0377-8398(02)00161-5.

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28

Salvi, Gianguido, Carla Buosi, Deborah Arbulla, et al. "Ostracoda and foraminifera response to a contaminated environment: the case of the Ex-Military Arsenal of the La Maddalena Harbour (Sardinia, Italy)." Micropaleontology 61, no. 1-2 (2015): 115–33. http://dx.doi.org/10.47894/mpal.61.1.09.

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Negative responses of biotic communities as trackers of pollutant dispersion has shown that microfaunal distribution can play a useful role in investigating marine coastal ecosystems. A detailed study was carried out on Ostracoda and benthic foraminiferal assemblages from the contaminated environment of the Ex-Military Arsenal of the La Maddalena Harbour, located on the south-eastern coast of La Maddalena Island (Sardinia, Italy), to investigate the responses to pollution of these micro-organisms in this area using integrated multidisciplinary approaches. The area is affected by industrial was
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29

MUNIZ, FELLIPE P., MARCOS CÉSAR BISSARO-JÚNIOR, EDSON GUILHERME, JONAS PEREIRA DE SOUZA FILHO, FRANCISCO RICARDO NEGRI, and ANNIE S. HSIOU. "VERTEBRATE TAPHONOMY OF TWO UPPER MIOCENE BONEBEDS IN WESTERN PROTO-AMAZONIA (SOLIMÕES FORMATION, BRAZIL): INSIGHTS FROM MACROVERTEBRATE AND MICROVERTEBRATE FOSSILS." PALAIOS 36, no. 8 (2021): 269–82. http://dx.doi.org/10.2110/palo.2021.020.

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ABSTRACT The Niterói and Talismã sites comprise two of the most important fossiliferous deposits of the Neogene in Brazil. After 30 years of research, these sites have revealed rich assemblages of vertebrates and provided a glimpse of the Amazonian fauna and environment during the Miocene. Despite this, detailed studies that attempt to explain the genesis of these bonebeds are still scarce and hamper more robust paleoenvironmental and paleoecological reconstructions. Here we provide the first in-depth taphonomic analysis for both locations. Sedimentological and taphonomic evidence suggest that
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30

Bernárdez, Patricia, Ricardo Prego, Manuel Varela, and Guillermo Francés. "Diatom thanatocoenosis in a middle Galician Ría: Spatial patterns and their relationship to the seasonal diatom cycle in the water column and hydrographic conditions." Continental Shelf Research 28, no. 17 (2008): 2496–508. http://dx.doi.org/10.1016/j.csr.2008.07.005.

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31

Ferrigno, Federica, Gabriella Di Martino, Luigia Donnarumma, et al. "Unexpected and Extraordinarily Shallow Coralligenous Banks at the Sinuessa Site, a Heritage of the Campania Coast (SW Italy, Mediterranean Sea)." Water 16, no. 20 (2024): 2942. http://dx.doi.org/10.3390/w16202942.

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Coralligenous bioconstructions are biogenic calcareous formations developing at low irradiance on littoral rocky cliffs or on the deeper sub-horizontal bottom in the Mediterranean Sea. Unusually shallow coralligenous banks on the sandy coast of Sinuessa (Mondragone City, Gulf of Gaeta, SW Italy) were investigated. Their communities and the surrounding biogenic detritus were characterized. Geophysical and acoustic data revealed the presence of coralligenous banks between 7.5 and 15 m depth, showing constant thickness and sub-horizontal geometry, incised by sub-perpendicular channels. Sediment d
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32

TAKAHASHI, Yutaka, and Itaru KOIZUMI. "Diatom thanatocoenoses in Hamana-ko Bay." Journal of the Geological Society of Japan 93, no. 6 (1987): 419–29. http://dx.doi.org/10.5575/geosoc.93.419.

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33

Zolotarev, Valentin, and Svetlana Stadnichenko. "Thanatocoenoses of mollusc shells in the north-western part of the Black Sea." GEO&BIO 2021, no. 20 (2021): 50–57. http://dx.doi.org/10.15407/gb2007.

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Following death, mollusc shells become elements of thanatocoenoses of bottom and coastal deposits. At the early stages of succession of storm strands, the conservation of mollusc shells in the coastal deposits is high, which allows to obtain a larger number of shells to determine their traits. The probability of finding shells of rare mollusc species in the coastal strands is significantly higher than in bottom grab samples. Therefore, the taxonomic composition of the thanatocoenoses may correspond to the actual composition of mollusc assemblage in the adjacent coastal waters. Determination of
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34

Stanik, Katarzyna, and Bronisław Wołoszyn. "Microevolution of Bechstein's Bat Myotis Bechsteinii (Kuhl, 1817) (Mammalia: Chiroptera) in the Holocene of Southern Poland." Travaux du Muséum National d'Histoire Naturelle "Grigore Antipa" 54, no. 1 (2011): 243–62. http://dx.doi.org/10.2478/v10191-011-0015-1.

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Microevolution of Bechstein's Bat Myotis Bechsteinii (Kuhl, 1817) (Mammalia: Chiroptera) in the Holocene of Southern Poland Bechstein's bat was one of the most common species in the Middle and Late Holocene of Southern Poland. It dominated in Kraków - Częstochowa Upland, but was also frequent in Tatra Mountains. Bone material from thanatocoenoses, dated by 14C AMS method, was analysed. The aim of studies was to investigate the direction of changes in skull and mandible morphology of Myotis bechsteinii during the period from 5710 BC till present day and to answer the question which environmenta
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35

Bhalla, S. N., and P. K. Kathal. "Recent foraminiferal thanatocoenoses from the Gulf of Mannar, India." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 207, no. 3 (1998): 419–31. http://dx.doi.org/10.1127/njgpa/207/1998/419.

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36

Tinn, Oive, and Tõnu Meidla. "Ontogeny and thanatocoenoses of early middle Ordovician palaeocope ostracode species Brezelina palmata (Krause, 1889) and Ogmoopsis bocki (Öpik, 1935)." Journal of Paleontology 77, no. 1 (2003): 64–72. http://dx.doi.org/10.1017/s0022336000043420.

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The ctenonotellid ostracode species Brezelina palmata (Krause, 1889) and the tetradellid species Ogmoopsis bocki (Öpik, 1935) are represented by seven and five molting stages, respectively. Both species display an association of velar and size dimorphism in the three last instars. The analysis of the juvenile morphology of O. bocki provides evidence for a close relationship with the earliest known palaeocope ostracode species Nanopsis nanella (Moberg and Segerberg, 1906). The population age structure of B. palmata in synchronous beds at two localities reveals different types of thanatocoenoses
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37

Martello, Alcemar R., Carla B. Kotzian, and Marcello G. Simões. "Quantitative fidelity of recent freshwater mollusk assemblages from the Touro Passo River, Rio Grande do Sul, Brazil." Iheringia. Série Zoologia 96, no. 4 (2006): 453–65. http://dx.doi.org/10.1590/s0073-47212006000400010.

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This study represents one of the first contributions to the knowledge on the quantitative fidelity of the recent freshwater molluscan assemblages in subtropical rivers. Thanatocoenoses and biocoenoses were studied in straight and meandering to braided sectors, in the middle course of the Touro Passo River, a fourth-order tributary of the Uruguay River, located in the westernmost part of the State of Rio Grande do Sul. Samplings were carried out through quadrats of 5 m², five in each sector. A total area of 50 m² was sampled. Samplings were also made in a lentic environment (abandoned meander),
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38

Uffenorde, Henning. "Living and Quaternary Ostracoda from the Eastern Adriatic Sea: Biocoenoses, thanatocoenoses or palaeothanatocoenoses?" Natura Croatica 25, no. 1 (2016): 73–86. http://dx.doi.org/10.20302/nc.2016.25.4.

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39

Čiliak, Marek, and Jozef Šteffek. "Vyhodnotenie malakofauny z náplavov Neresnice (stredné Slovensko) [Interpretation of molluscan fauna from the Neresnica River flood deposits (Central Slovakia)]." Malacologica Bohemoslovaca 10 (November 23, 2011): 73–78. https://doi.org/10.5817/MaB2011-10-73.

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Sampling of flood debris deposits can be useful method in insufficiently surveyed areas. This sampling method also allows us to detect the presence of rare and endangered species in the study area. We studied flood debris along the Neresnica River to gather data on mollusc fauna of the Pliešovská Kotlina basin and the Javorie Mts. (Central Slovakia). In spring 2010, samples of flood debris were taken at three sites along the river. Molluscan thanatocoenoses were composed of 68 species (56 terrestrial and 12 aquatic ones). The most notable records were two subterranean species &nd
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Tchoumatchenco, Platon Vassilev. "Brachiopod thanatocoenoses in the Aalenian, Bajocian and Bathonian of western Bulgaria and their distribution." Palaeogeography, Palaeoclimatology, Palaeoecology 100, no. 1-2 (1993): 159–68. http://dx.doi.org/10.1016/0031-0182(93)90039-l.

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LUTAENKO, KONSTANTIN A. "Beach Molluscan Thanatocoenoses in Possjet Bay, Sea of Japan: Comparison between Open and Sheltered Beaches." BENTHOS RESEARCH 1994, no. 47 (1994): 1–12. http://dx.doi.org/10.5179/benthos1990.1994.47_1.

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42

Taviani, M., P. Bouchet, B. Metivier, M. Fontugne, and G. Delibrias. "Intermediate steps of southwards faunal shifts testified by last glacial submerged thanatocoenoses in the Atlantic ocean." Palaeogeography, Palaeoclimatology, Palaeoecology 86, no. 3-4 (1991): 331–38. http://dx.doi.org/10.1016/0031-0182(91)90089-a.

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43

Čiliak, Marek, and Jozef Šteffek. "Vyhodnotenie malakofauny z náplavov Neresnice (stredné Slovensko) [Interpretation of molluscan fauna from the Neresnica River flood deposits (Central Slovakia)]." Malacologica Bohemoslovaca 10 (November 23, 2011): 73–78. http://dx.doi.org/10.5817/mab2011-10-73.

Full text
Abstract:
Sampling of flood debris deposits can be useful method in insufficiently surveyed areas. This sampling method also allows us to detect the presence of rare and endangered species in the study area. We studied flood debris along the Neresnica River to gather data on mollusc fauna of the Pliešovská Kotlina basin and the Javorie Mts. (Central Slovakia). In spring 2010, samples of flood debris were taken at three sites along the river. Molluscan thanatocoenoses were composed of 68 species (56 terrestrial and 12 aquatic ones). The most notable records were two subterranean species – Lucilla scintil
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44

Molina-Cruz, A., L. Welling, and A. Caudillo-Bohorquez. "Radiolarian distribution in the water column, southern Gulf of California, and its implication in thanatocoenose constitution." Marine Micropaleontology 37, no. 2 (1999): 149–71. http://dx.doi.org/10.1016/s0377-8398(99)00030-4.

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TINN, OIVE, and TÕNU MEIDLA. "ONTOGENY AND THANATOCOENOSES OF EARLY MIDDLE ORDOVICIAN PALAEOCOPE OSTRACODE SPECIES BREZELINA PALMATA (KRAUSE, 1889) AND OGMOOPSIS BOCKI (ÖPIK, 1935)." Journal of Paleontology 77, no. 1 (2003): 64–72. http://dx.doi.org/10.1666/0022-3360(2003)077<0064:oatoem>2.0.co;2.

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Duros, P., F. J. Jorissen, F. Cesbron, et al. "Benthic foraminiferal thanatocoenoses from the Cap-Ferret Canyon area (NE Atlantic): A complex interplay between hydro-sedimentary and biological processes." Deep Sea Research Part II: Topical Studies in Oceanography 104 (June 2014): 145–63. http://dx.doi.org/10.1016/j.dsr2.2013.09.024.

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Ayala-López, Adriana, and Adolfo Molina-Cruz. "Micropalaeontology of the hydrothermal region in the Guaymas Basin, Mexico." Journal of Micropalaeontology 13, no. 2 (1994): 133–46. http://dx.doi.org/10.1144/jm.13.2.133.

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Abstract. A micropalaeontological analysis of 40 sedimentary samples from a hydrothermal region in the Guaymas Basin, Gulf of California, Mexico, was carried out to describe microenvironments. These microenvironments were defined through a Q-mode Factor analysis of species abundance data from the benthic foraminiferal biocoenoses and thanatocoenoses. The benthic foraminiferal results were correlated with the biogeographic patterns of diatoms, radiolarians, planktonic foraminifers and ostracods through a ‘graphic-multivariate analysis’. Although the microenvironments have a patchy distribution
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Postawa, Tomasz. "Changes in Bat Fauna During the Middle and Late Holocene as Exemplified by Thanatocoenoses Dated with14C AMS from Kraków-Częstochowa Upland Caves, Poland." Acta Chiropterologica 6, no. 2 (2004): 269–92. http://dx.doi.org/10.3161/001.006.0206.

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Medioli, F. S., C. T. Schafer, and D. B. Scott. "Distribution of recent benthonic foraminifera near Sable Island, Nova Scotia." Canadian Journal of Earth Sciences 23, no. 7 (1986): 985–1000. http://dx.doi.org/10.1139/e86-100.

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Sable Island is a 38 km long feature that is situated near the outer margin of the Scotian Shelf between George's Bank and the Laurentian Channel. Grab samples of the predominantly sandy substrate that surrounds the island's offshore areas were collected from water depths of 0 to ~55 m.Textural data indicate that winnowing processes are comparatively intense in offshore areas, especially on the north side of the island. A higher frequency of samples containing more than 2% clay-size particles occurs in an area lying off the southeastern coast of the island. The clay suggests that a pre-Recent
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Sapunov, Ivo, Platon Tchoumatchenco, and Vladimir Shopov. "The Lower Jurassic in the Troyan Region and the south-eastern part of the Teteven Region, Central Balkanids (brachiopod-, bivalve-, and ammonite stratigraphy and palaeotectonics)." Geologica Balcanica 26, no. 3 (1996): 3–19. http://dx.doi.org/10.52321/geolbalc.26.3.3.

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As a result of the biostratigraphic study of brachiopods, bivalves and ammonites made in eight instructive sections it was established that most of the Lower Jurassic rock sequences were more or less incomplete. The sections in the valleys of the rivers Kostina and Cherna Reka, Teteven Region, are most complete (from Hettangian to Toarcian). They are situated in the central, the most deeply sinking block one – called Kostina Step of the Izdremets Complex Graben of the Moesian Early-Middle Jurassic Platform. There, the most deep-sea Early Jurassic distal facies were existing. The section near t
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