Academic literature on the topic 'Foraminiferos'
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Journal articles on the topic "Foraminiferos"
Glock, Nicolaas, Julia Wukovits, and Alexandra-Sophie Roy. "Interactions of Globobulimina Auriculata with Nematodes: Predator Or Prey?" Journal of Foraminiferal Research 49, no. 1 (January 11, 2019): 66–75. http://dx.doi.org/10.2113/gsjfr.49.1.66.
Full textRoy, T., F. Lombard, L. Bopp, and M. Gehlen. "Projected impacts of climate change and ocean acidification on the global biogeography of planktonic Foraminifera." Biogeosciences 12, no. 10 (May 19, 2015): 2873–89. http://dx.doi.org/10.5194/bg-12-2873-2015.
Full textSenowbari-Daryan, Baba, and Michael Link. "Foraminifera from the Norian–Rhaetian reef carbonates of the Taurus Mountains (Saklıkent, Turkey)." Geologica Carpathica 68, no. 4 (August 1, 2017): 303–17. http://dx.doi.org/10.1515/geoca-2017-0021.
Full textGlock, Nicolaas, Alexandra-Sophie Roy, Dennis Romero, Tanita Wein, Julia Weissenbach, Niels Peter Revsbech, Signe Høgslund, David Clemens, Stefan Sommer, and Tal Dagan. "Metabolic preference of nitrate over oxygen as an electron acceptor in foraminifera from the Peruvian oxygen minimum zone." Proceedings of the National Academy of Sciences 116, no. 8 (February 6, 2019): 2860–65. http://dx.doi.org/10.1073/pnas.1813887116.
Full textMartinez, Ana, Laura Hernández-Terrones, Mario Rebolledo-Vieyra, and Adina Paytan. "Impact of carbonate saturation on large Caribbean benthic foraminifera assemblages." Biogeosciences 15, no. 22 (November 16, 2018): 6819–32. http://dx.doi.org/10.5194/bg-15-6819-2018.
Full textRoy, T., F. Lombard, L. Bopp, and M. Gehlen. "Projected impacts of climate change and ocean acidification on the global biogeography of planktonic foraminifera." Biogeosciences Discussions 11, no. 6 (June 30, 2014): 10083–121. http://dx.doi.org/10.5194/bgd-11-10083-2014.
Full textPearson, Paul N. "Oxygen Isotopes in Foraminifera: Overview and Historical Review." Paleontological Society Papers 18 (November 2012): 1–38. http://dx.doi.org/10.1017/s1089332600002539.
Full textKeul, N., G. Langer, L. J. de Nooijer, and J. Bijma. "Effect of ocean acidification on the benthic foraminifera <i>Ammonia</i> sp. is caused by a decrease in carbonate ion concentration." Biogeosciences 10, no. 10 (October 1, 2013): 6185–98. http://dx.doi.org/10.5194/bg-10-6185-2013.
Full textNatsir, Suhartati M. "THE DISTRIBUTION OF BENTHIC FORAMINIFERA IN DAMAR ISLAND AND JUKUNG ISLAND, SERIBU ISLANDS." Marine Research in Indonesia 35, no. 2 (December 31, 2010): 9. http://dx.doi.org/10.14203/mri.v35i1.10.
Full textNatsir, Suhartati M. "THE DISTRIBUTION OF BENTHIC FORAMINIFERA IN DAMAR ISLAND AND JUKUNG ISLAND, SERIBU ISLANDS." Marine Research in Indonesia 35, no. 2 (December 31, 2010): 9–14. http://dx.doi.org/10.14203/mri.v35i2.10.
Full textDissertations / Theses on the topic "Foraminiferos"
Arriaga, Cavalieri Maria Eugenia. "Patrones de supervivencia y recuperación de los macroforaminíferos después de la extinción en masa del límite Cenomaniense-Turoniense." Doctoral thesis, Universitat Autònoma de Barcelona, 2016. http://hdl.handle.net/10803/394041.
Full textLarger foraminifera are a k-strategists group extremely abundant in shallow water plat¬form environments, both in the recent and the fossil record. They represent one of the most sensitive marine organisms to environmental perturbations. During the Cenomanian-Turonian Boundary (CTB) interval, coinciding with a widespread episode of organic-rich sediments deposition (Oceanic Anoxic Event 2 or Bonarelli event), the larger foraminifera inhabiting the shallow environment were dramatically affected by a major paleoenvironmental conditions change. Such event finished with the middle Cretaceous Glo¬bal Community Maturation Cycle (GCMC). In this work we discuss the post-extinction recovery pattern. This works has been carried out in two neighboring paleoprovinces: Central Tethys, which outcrop at the southern Appenines, and the Pyrenean, outcrop located at the southern Pyrenees (Central Sud-pyrenean Unit). In the Pyrenees, like in most of the platforms, the water layer suffered an eutrophication process that leads demise the carbonate producer organisms, causing a stop on carbonate sedimentation. Such lack on sedimentation generates a sedimen¬tary hiatus perceptible in the stratigraphic record before the drowning episode. While the platform from southern Apennines was able to keep up on shallow carbonate sedimentation, and despite the colonization of cyanobacteria organisms, some small foraminifera were capa¬ble to survive. Here is suggest that even though the paleogeographic and depositional differences bet¬ween the studied areas, both present similar recovery patterns in the fallowing way: 1) The genetic information necessary for sustaining a k-strategy was lost with the extinction, but the “legacy” of larger foraminifera survived in the small r-strategist forms of Nezzazatinella, Cu¬neolina, Dictyopsella and Rotorbinella survivor genus. 2) chronostratigraphic calibration of Apenninic sections made by Strontium and Carbon Isotopic Stratigraphic data, indicates that the firth “newcomers ” appears during the upper part of lower Turonian with Moncharmontia apenninica and Pseudocyclammina spharoidea new species; but is not until middle-upper Tu¬ronian that more complex forms appears with Scandonea samnítica and Reticulinella kaeveri species. 3) In the Pyrenees, the shallow foraminiferal fauna reenter during the mid-upper Tu¬ronian after the carbonate sedimentation retrieval, represented by Moncharmontia apennini¬ca and Pseudocyclammina spharoidea species together with the “legacy” forms from Cenoma¬nian age; then also appear more complex genus as Eofallotia. 4) It seems like in both areas the Global Community Maduration Cycle of upper Cretaceous began simultaneously. However, from the middle-upper some sort of provincialism is noticeable with the presence of Scando¬nea and Reticulinella genus in the central Tethys, while the firth forms of meandropsinids are showns up for the Pyrenean realm, such paleoprovincialism considerably emphasizes during the latter stages of upper Cretaceous GCMC.
Silva, Cristiane Pakulski da. "Bioestratigrafia e paleoecologia de foraminíferos da Bacia de Barreirinhas, cretácio, margem equatorial brasileira." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2011. http://hdl.handle.net/10183/38528.
Full textThis study integrates biostratigraphic and paleoecological information obtained through of planktonic and benthic foraminifera analysis from sediment recovered from five wells (1-MAS-1, 1-MAS-3A, 1-MAS-4A, 1-MAS-14 and 1-MAS-15) of Barreirinhas Basin, making a total of 127 samples prepared and analyzed. The sediments analyzed here cover the upper Albian to upper Campanian stages with geological record inserted in the Caju (Albian - Cenomanian) and Humberto de Campos (Turonian - Maastrichtian) groups. Through the biostratigraphic data obtained it was possible to establish seven foraminiferal biozones, of local character, based on the last occurrence of taxon guide (LAD - Last Appereance Datum). The upper Albian was defined based on planktonic foraminifera biozones of Ticinella primula Lauterbacher (1963) and benthic foraminifera Lingulogavelinella albiensis Malapris (1965)-Gyroidina Bandy Trujillo (1960); the lower Cenomanian was determined through the planktonic foraminifera biozones of Globigerinelloides bentonensis Morrow (1934) and benthic foraminifera Coronorotalites aptiensis Bettenstaedt (1952); the upper Cenomanian was recognized through the planktonic foraminifera biozones of Rotalipora appeninica Renz (1936) and benthic foraminifera Gavelinella intermedia Berthelin (1880); the upper Campanian was determined based on the planktonic foraminifera biozone Heterohelix pulchra Brotzen (1936). After the identification of microfauna, was possible to recognize 108 species of foraminifera belonging to five suborders: the Suborder Globigerinina, of planktonic foraminifera, is represented by 40 species and 15 genera; the benthic foraminifera are composed of 68 species and 48 genera, belonging to the suborders Rotaliina, Textulariina, Lagenina and Miliolina. Through analysis of foraminifera assemblage it was possible to trace the CCD (Carbonate Compensation Depth) in the wells and separate them based on depth in: distal (1-MAS-1 and 1-MAS-14) and proximal (1-MAS-3A, 1-MAS-4A and 1-MAS-15). It was noted that the Barreirinhas Basin has an overall transgression during the Cretaceous Period, characterized by sedimentary influx through weather changes, like global warming that occurred during this period. This theory is enhanced by the complete absence of calcareous tests, both of benthic as planktonic foraminifera associated with the exclusive occurrence of agglutinating and arenaceous benthic (Reophax globosus) in the distal wells of the end of Cretaceous Period. In the wells 1-MAS-3A, 1-MAS-4A and 1-MAS-15, the foraminifera fauna identified presents morphological adaptations to conditions of low oxygen in the water column, features typically seen during the Oceanic Anoxic Event (OEA's). As examples of these morphological adaptations, was identified three species of the Schakoina genera, which has elongated chambers and Biticinella breggiensis species, which has bilobeted chambers, suggesting an increase in the primary productivity, nutrient availability and paleoenvironments depleted in oxygen. Based on this information it was possible to identify a local character anoxic events occurred during the upper Albian, recorded only in a well 1-MAS-3A and 1-MAS-4A, while the global anoxic event 2 was recorded in a well 1-MAS-15.
Zerfass, Geise de Santana dos Anjos. "Estudos paleoambientais com base em isótopos de carbono, oxigênio e estrôncio em foraminíferos do terciário da Bacia de Pelotas." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2009. http://hdl.handle.net/10183/23713.
Full textThe Pelotas Basin, situated in the southern Brazilian Atlantic Margin, is filled with siliciclastic sediments deposited from Cretaceous to Holocene. The absence of volcanic strata appropriate to radiometric dating and the abundance of calcareous microfossils constitute a favorable scenario for the use of strontium isotope ratio to obtain chronostratigraphic data for the Tertiary section of the basin. Furthermore, the conspicuous occurrence of organic-walled microfossils makes this section suitable for biochronostratigraphic correlations. A synthesis of the biostratigraphic data published is presented in order to recognize discontinuities in the stratigraphic record. Afterward, the assessment of the foraminifera tests preservation was effectuated with the purpose of providing criteria to select the samples to be analyzed and verify the consistency of the isotopic data. Four types of diagenetic alterations were recognized in different stratigraphic levels, from the base to the top of the studied section: recrystallization, cementation, oxidized coatings and dissolution. Strontium, oxygen and carbon isotope ratios and Sr/Ca ratio were performed in foraminifera tests from four drill-holes. Foraminifera and palynomorphs recovered from cores of two wells located on onshore and offshore regions provided a biostratigraphic and paleoenvironmental information, constituting a reference section for correlation. Based on the core study, a highresolution biostratigraphic framework is proposed, in which a hiatus of 2 Ma is identified in the middle Miocene, as well as a transgressive event in the middle-late Miocene. In a broader approach, a chronostratigraphic framework is presented for the Paleogene-Neogene section of four drill-holes. Six hiatuses were recognized: (i) Paleocene, (ii) early-middle Eocene, (iii) middle Eocene, (iv) late Eocene - early Oligocene, (v) early Miocene, and (vi) early Miocene - middle/late Miocene. The identified hiatuses, except that of early-middle Eocene, were interpreted as disconformities in association with global events. A sea-level fall at 10.4 Ma may be related to the deposition of Rio Grande Cone. Global eustatic sea-level falls produced the disconfomities recognized at 18.5 Ma, 31.5 Ma and 40.5 Ma. The hiatus recognized in the early Eocene was interpreted as a condensed-section deposited between 53.7 and 47.9 Ma. From the early Eocene to the late Oligocene, a trend of cooling registered using oxygen and carbon isotopes may be related to the opening of the Drake Passage. Based on δ13C, a trend of increasing productivity probable driven by warming was observed from the late Oligocene to the early Miocene. Another cooling phase was registered in the late Miocene section which can be related to the reestablishment of the ice-sheet in Antarctica. This interval is punctuated of short-term cycles of approximately 400 ky.
Nagai, Renata Hanae. "Variações de paleoprodutividade na plataforma interna de Cabo Frio, RJ, durante o holoceno." Universidade de São Paulo, 2009. http://www.teses.usp.br/teses/disponiveis/21/21133/tde-24092009-111219/.
Full textSedimentological, geochemical and benthic foraminifera analyses carried out on a core sampled from the inner shelf of Cabo Frio, enabled us to identify different four productivity regimes related to sea-level fluctuations and/or climatic changes, that occurred in the southeastern Brazilian continental margin, during the last 9.3 kyr cal BP. Prior to 7.0 kyr cal BP, a lower productivity and less intense hydrodynamic regime occurred at lower sea levels and under drier climatic conditions. Between 7.0 and 5.8 kyr cal BP, relatively stronger local oceanic circulation and relatively high productivity were observed, in a scenario of rising sea levels and more humid conditions. From 5.8 to 2.8 kyr cal BP, bottom currents weakened and input of nutrients increased, with productivity levels similar to the previous phase at lower sea level and in a drier climate. From 2.8 kyr cal BP up to the present, stronger hydrodynamic conditions and a higher productivity regime linked to the establishment of the upwelling process in Cabo Frio. From 2.5 kyr cal BP to the present, upwelling enhancement has been recognized, resulting from the combined action of NE winds (related to El- Niño events and/or the Intertropical Convergence Zone - ITCZ - position), the meandering pattern of the Brazilian Current - BC - and present day coastline configuration.
Disaró, Sibelle Trevisan. "Caracterização da plataforma continental da Bacia de Campos (Brasil, SE) fundamentada em foraminíferos bentônicos recentes." reponame:Biblioteca Digital de Teses e Dissertações da UFRGS, 2014. http://hdl.handle.net/10183/172465.
Full textSpatial and seasonal differences over the continental shelf and along the shelf break edges of Campos Basin, southeastern Brazil (20.5°S - 24°S) were investigated during 2008 (downwelling setting/dry/winter) and 2009 (upwelling setting/rainy/summer), based on living benthic foraminiferal assemblages, as part of the “HABITATS Project - Evaluation of the Environmental Heterogeneity of the Campos Basin, Brazil”. The assemblages and their relationship with environmental variables were studied to support the research and development activities of PETROBRAS, the Brazilian state-owned oil Company. The sampling design consisted of nine transects (45 stations) perpendicular to the coastline. Three replicates were taken from each station using a modified grab that performs as a box corer. The surface (0-2 cm) bottom sediment was collected (10 cm x 10 cm), fixed with 4 % formaldehyde buffered solution, stained with Bengal Rose, washed and sieved through a 63 μm mesh. Of the 200 cm3 of each replicate, 20 cm³ were analyzed and the remainder stored for retesting. Foraminiferal assemblages were recognized using cluster analysis, indicator species analysis and nonmetric multidimensional scaling. Spatial and temporal patterns of the foraminiferal assemblages were identified and the ecological structure (density, diversity, dominance, equitability) of these assemblages investigated. Foraminiferal biomass was estimated by measuring biovolume. The correlations of biotic and abiotic parameters were evaluated using canonical correspondence analysis. A total of 519 foraminiferal taxa were recorded. Spatial distribution responds to depth, sediment (grain size and carbonate content) and food availability. Cluster analysis with integrated periods allowed the recognition of three distinct areas: (i) an Inner shelf (25 – 50 m) area positively correlated with sand, higher temperature and higher chlorophyll-a content; it was occupied by Tiphotrocha concava, Bolivina paula, Nonionella sp. C, Discorbis williamsoni, Ammonia parkinsoniana, Ammonia tepida, Bolivina striatula, Textularia agglutinans, Angulogerina cf. A. jamaicensis, Buliminella elegantissima, Paracassidulina nipponensis, Rectocibicides miocenicus, Placopsilina bradyi and species of Quinqueloculina, Textularia, Asterotrochammina, Eoeponidella, Porosononion, Polymorphina, Rotaliammina and Discorbis. (ii) a Medium/outer shelf (75 – 150 m) area is composed by two subgroups correlated with depth and elevated carbonate levels; its species association includes Uvigerina auberiana, Technitella harrisii, Paratrochammina brasiliensis s.l., Planulina foveolata, Seabrookia earlandi, Svratkina spp., Pullenia spp., Eponides antillarum, Discorbinella floridensis, Cibicidoides corpulentus, Stomatorbina torrei, Labrospira jeffreysii, Tetrataxiella ayalai, Mychostomina revertens, Amphicoryna scalaris, Globocassidulina rossensis, Ehrenbergina spinea, Spirotextularia floridana, Siphonina reticulata, Spirillina vivipara, Patellina corrugata and some species from Astrononion, Fissurina and Lenticulina. (iii) an Upwelling area is positively correlated with phaeopigment (phytodetritus), mud and total organic carbon; this group includes abundant small rotalids such as Bulimina marginata, Pappina compressa, Angulogerina angulosa, s.l., Alabaminella weddellensis, Bolivina fragilis, Bolivina ordinaria, Nonionella stella, Hopkinsina pacifica, Bolivinellina translucens, Stainforthia complanata, Bulimina patagonica, Hanzawaia concentrica, Gyroidina umbonata, Nonionella opima, Epistominella exigua, Cassidulina carinata, Fursenkoina pontoni and Nonionella atlantica, and such agglutinated foraminifers as Adercotryma glomeratum, Lagenammina atlantica, Ammoscalaria pseudospiralis, Reophax scorpiurus, Sepetibaella sepetibaensis, Labrospira crassimargo, Reophax pauciloculatus, Leptohalysis scottii, Textularia ? torquata, Pseudobolivina fusiformis and Reophax arayaensis, and some miliolids (Quinqueloculina sabulosa, Quinqueloculina atlantica s.l. and Pyrgo nasuta). During the upwelling period the South Atlantic Coastal Waters enlarged its influence to include not only the Cape Frio area, but also an area at about 75 meters depth off Cape Sao Tome. Biomass values at the inner shelf agreed with available published data, but on the middle and outer shelf the values are higher than expected for an oligotrophic, seasonally mesotrophic basin. The ABC curves indicate the 25 m isobath as the most disturbed one and recognize a moderated disturbance in the upwelling area. During rainy season the 25 m isobath is disturbed by natural eutrophication phenomena that may be significantly amplified by anthropogenic activities. This study provides data for the monitoring plan for the area and for paleoenvironmental reconstructions.
Bowen, Powell Jacqueline. "Larger Foraminiferal Biostratigraphy, Systematics And Paleoenvironments of The Avon Park Formation and Ocala Limestone, Highlands County, Florida." FIU Digital Commons, 2010. http://digitalcommons.fiu.edu/etd/288.
Full textMayer, Michaela. "Zur Ökologie der Benthos-Foraminiferen der Potter Cove (King George Island, Antarktis) = Ecology of benthic foraminifera in the Potter Cove (King George Island, Antarctica) /." Bremerhaven : Alfred-Wegener-Institut für Polar- und Meeresforschung, 2000. http://www.gbv.de/dms/bs/toc/314065083.pdf.
Full textVarhelyi, Aron. "Quaternary Arctic foraminiferal isotopes: species reliability and palaeoceanographic application." Thesis, Stockholms universitet, Institutionen för geologiska vetenskaper, 2018. http://urn.kb.se/resolve?urn=urn:nbn:se:su:diva-158047.
Full textMed siktet på att undersöka huruvida variationer i stabila isotopvärden (δ18O/δ13C) hos foraminiferer har potential som dateringsredskap i Arktiska Oceanen, presenteras härmed ny δ18O/δ13C data från fem marina sedimentkärnor. Tre kärnor analyseras på längden (PS92/54-1; LOMROG III TC/PC-03 och PC-07) medan två analyser begränsas till kärnornas toppskikt (LOMROG I PC-04 och PC-08). Resultat från sju olika arter av bentoniska foraminiferer (Cassidulina neoteretis, Cibicides lobatulus, Cibicidoides wuellerstorfi, Oridorsalis tener, Quinqueloculina arctica, Stainforthia concava and Triloculina sp.) och en planktonisk (Neogloboquadrina pachyderma sinistral) har jämförts mot data som baserats på kärnornas fysiska egenskaper, mängden foraminiferer och befintliga åldersberäkningar. De nya isotopresultaten avslöjar nischer som är specifika för varje art och som, förutom isotopvärdena i det omkringliggande havsvattnet, är beroende av varierande fraktioneringseffekter samt habitatpreferenser. Förändringar i δ13C är mestadels avhängigt paleoproduktivitet och gasutbyte mellan atmosfär och hav. Det har därför begränsad användning som dateringsredskap. Fokus har istället legat på att skapa högupplöst δ18O data som kan jämföras med en global δ18O ’stack’. Cibicidoides wuellerstorfi är den vanligast förekommande arten i TC/PC-03 och PC-07 medan C. neoteretis och N. pachyderma har flest förekomster i PS92/54-1. I den senare kärnan saknas C. neoteretis under perioder där förändringar i δ18O antas vara stora (interglacialer). Istället är det δ18O hos planktoniska N. pachyderma som i högst grad efterliknar en global bentonisk ’stack’. Dessa resultat antyder att N. pachyderma potentiellt kan användas som lokalt dateringsverktyg. För att kunna korrelera mot mer avlägsna sedimentkärnor i Arktiska Oceanen med hjälp av δ18O från N. pachyderma, så behöver hänsyn tas till regionala skillnader i pelagial δ18O, varierande kalcifieringsdjup och dålig bevaring av foraminifererna. Det är viktigt att adressera varför det finns en amplitudskillnad mellan olika sedimentkärnor för samma tidsperioder, innan försök görs att sammanfoga δ18O resultat från den vanligt förekommande Arktiska bentoniska arten C. neoteretis.
Licari, Laetitia. "Ecological preferences of Benthic Foraminifera in the Eastern South Atlantic : distribution patterns, stable carbon isotopic composition, and paleoceanographic implications = Ökologische Ansprüche benthischer Foraminiferen im östlichen Südatlantik /." Bremerhaven : Alfred-Wegener-Inst. für Polar- und Meeresforschung, 2006. http://www.gbv.de/dms/bs/toc/514912308.pdf.
Full textKuhn, Winfried. "Paleozäne und untereozäne Benthos-Foraminiferen des bayerischen und salzburgischen Helvetikums - Systematik, Stratigraphie und Palökologie /." München : F. Pfeil, 1992. http://catalogue.bnf.fr/ark:/12148/cb37429165g.
Full textBooks on the topic "Foraminiferos"
Mikhalevich, V. I. Sistema chetyrekh podklassov foraminifer s aggli͡utinirovannoĭ stenkoĭ rakovin (Ammodiscana, Miliamminana, Hormosinana, Textulariana) (Foraminifera). Sankt-Peterburg: Zoologicheskiĭ in-tut RAN, 2003.
Find full textEvolution and geological significance of larger benthic foraminifera. Amsterdam: Elsevier, 2008.
Find full textMackensen, Andreas. Zur Paläoozeanographie hoher Breiten: Stellvertreterdaten aus Foraminiferen = Foraminiferal proxies : constraints on their use in high latitude paleoceanography. Bremerhaven: Alfred-Wegener-Institut, 1997.
Find full textSen Gupta, Barun K. Modern Foraminifera. Dordrecht: Springer Netherlands, 2003. http://dx.doi.org/10.1007/0-306-48104-9.
Full textCimerman, Franc. Mediterranean Foraminifera. Ljubljana: Slovenska akademija znanosti in umetnosti, 1991.
Find full textSchumacher, Stefanie. Mikrohabitatansprüche benthischer Foraminiferen in Sedimenten des Südatlantiks =: Microhabitat preferences of benthic foraminifera in South Atlantic Ocean sediments. Bremerhaven: Alfred-Wegener-Institut für Polar- und Meeresforschung, 2001.
Find full textBeck Eichler, Patrícia Pinheiro, and Christofer Paul Barker. Benthic Foraminiferal Ecology. Cham: Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-61463-8.
Full textNuglisch, Klaus. Foraminiferen, marine Mikroorganismen. Wittenberg Lutherstadt: A. Ziemsen, 1985.
Find full textKouwenhoven, Tanja J. Survival under stress: Benthic foraminiferal patterns and Cenozoic biotic crises = Overleven onder stress : benthonische foraminiferen en Cenozoische biotische crises. [Utrecht]: Faculteit Aardwetenschappen, Universiteit Utrecht, 2000.
Find full textKouwenhoven, Tanja J. Survival under stress: Benthic foraminiferal patterns and Cenozoic biotic crises = Overleven onder stress : benthonische foraminiferen en Cenozoische biotische crises. [Utrecht]: Faculteit Aardwetenschappen, Universiteit Utrecht, 2000.
Find full textBook chapters on the topic "Foraminiferos"
Edwards, Robin, and Alex Wright. "Foraminifera." In Handbook of Sea-Level Research, 191–217. Chichester, UK: John Wiley & Sons, Ltd, 2015. http://dx.doi.org/10.1002/9781118452547.ch13.
Full textCortés, Jorge, Claudia Mora-Baumgartner, and Vanessa Nielsen. "Foraminifera." In Marine Biodiversity of Costa Rica, Central America, 131–35. Dordrecht: Springer Netherlands, 2009. http://dx.doi.org/10.1007/978-1-4020-8278-8_8.
Full textAltenbach, Alexander V. "Foraminifera." In Encyclopedia of Geobiology, 393–96. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-1-4020-9212-1_93.
Full textHallock, Pamela. "Foraminifera." In Encyclopedia of Modern Coral Reefs, 416–21. Dordrecht: Springer Netherlands, 2011. http://dx.doi.org/10.1007/978-90-481-2639-2_80.
Full textArmstrong, Howard A., and Martin D. Brasier. "Foraminifera." In Microfossils, 142–87. Malden, MA USA: Blackwell Publishing, 2013. http://dx.doi.org/10.1002/9781118685440.ch15.
Full textSabbatini, Anna, Caterina Morigi, Maria Pia Nardelli, and Alessandra Negri. "Foraminifera." In The Mediterranean Sea, 237–56. Dordrecht: Springer Netherlands, 2013. http://dx.doi.org/10.1007/978-94-007-6704-1_13.
Full textEhrlich, Hermann. "Foraminifera." In Biological Materials of Marine Origin, 455–64. Dordrecht: Springer Netherlands, 2010. http://dx.doi.org/10.1007/978-90-481-9130-7_33.
Full textBinczewska, Anna, Irina Polovodova Asteman, and Elizabeth J. Farmer. "Foraminifers (Benthic)." In Encyclopedia of Marine Geosciences, 1–8. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6644-0_60-1.
Full textBoltovskoy, Demetrio, and Nancy Correa. "Foraminifers (Planktonic)." In Encyclopedia of Marine Geosciences, 1–9. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6644-0_61-4.
Full textBoltovskoy, Demetrio, and Nancy Correa. "Foraminifers (Planktonic)." In Encyclopedia of Marine Geosciences, 1–9. Dordrecht: Springer Netherlands, 2015. http://dx.doi.org/10.1007/978-94-007-6644-0_61-5.
Full textConference papers on the topic "Foraminiferos"
Romanova, Alexandra, Alexandra Romanova, Vladimir Anin, Vladimir Anin, Sergey Pletnev, Sergey Pletnev, Tatyana Tarasova, and Tatyana Tarasova. "CARBONATE DISSOLUTION AND ULTRASTRUCTURAL BREAKDOWN IN PLANKTONIC FORAMINIFERA IN THE SEA OF OKHOTSK." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.21610/conferencearticle_58b4315c3db34.
Full textRomanova, Alexandra, Alexandra Romanova, Vladimir Anin, Vladimir Anin, Sergey Pletnev, Sergey Pletnev, Tatyana Tarasova, and Tatyana Tarasova. "CARBONATE DISSOLUTION AND ULTRASTRUCTURAL BREAKDOWN IN PLANKTONIC FORAMINIFERA IN THE SEA OF OKHOTSK." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b93b6ac2b30.99187085.
Full textRomanova, Alexandra, Alexandra Romanova, Vladimir Anin, Vladimir Anin, Sergey Pletnev, Sergey Pletnev, Tatyana Tarasova, and Tatyana Tarasova. "CARBONATE DISSOLUTION AND ULTRASTRUCTURAL BREAKDOWN IN PLANKTONIC FORAMINIFERA IN THE SEA OF OKHOTSK." In Managing risks to coastal regions and communities in a changing world. Academus Publishing, 2017. http://dx.doi.org/10.31519/conferencearticle_5b1b93cfe35991.48973379.
Full textMitacchione, V., and M. Odehnal. "Foraminiferos Grandes del Oligoceno Tardio Y Sistemas Sedimentarios Asociados en el Area de Boqueron, Venezuela Oriental." In 5th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609-pdb.116.025esp.
Full textCastro Mora, M. "Estudios por Nannoplancton Calcareo del Mioceno Temprano del Norte de Venezuela Comparado con las Localidades Tipo Para Foraminiferos Plancticos en La Isla de Trinidad." In 5th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609-pdb.116.022esp.
Full textGalea Allvarez, F. A., and J. Moreno Vásquez. "Biofacies de Foraminiferos en la Formacion Carapita Y su Relacion con los Eventos Tectonicos (Mioceno Temprano-Mioceno Medio) en el Norte de Monagas, Venezuela." In 5th Simposio Bolivariano - Exploracion Petrolera en las Cuencas Subandinas. European Association of Geoscientists & Engineers, 1994. http://dx.doi.org/10.3997/2214-4609-pdb.116.024esp.
Full textZaychikova, Ekaterina V. "Biostratigraphy of the upper jurassic of the Verkh-Tarskaya drilling area (South of Western Siberia in foraminifera)." In Недропользование. Горное дело. Направления и технологии поиска, разведки и разработки месторождений полезных ископаемых. Экономика. Геоэкология. Федеральное государственное бюджетное учреждение науки Институт нефтегазовой геологии и геофизики им. А.А. Трофимука Сибирского отделения Российской академии наук, 2020. http://dx.doi.org/10.18303/b978-5-4262-0102-6-2020-009.
Full textSadooni, Fadhil N., Hamad Al-Saad Al-Kuwari, Ahmad Sakhaee-Pour, and Wael S. Matter. "Linking Depositional Environments and Diagenetic Processes to Porosity Evolution and destruction in the Arab Formation reservoirs, Offshore oilfields of Qatar." In Qatar University Annual Research Forum & Exhibition. Qatar University Press, 2020. http://dx.doi.org/10.29117/quarfe.2020.0043.
Full textPoirier, Robert, Madison Q. Gaetano, Kimberly Acevedo, Morgan F. Schaller, Maureen E. Raymo, and Reinhard Kozdon. "QUANTIFYING DIAGENESIS, CONTRIBUTING FACTORS, AND RESULTING ISOTOPIC BIAS IN BENTHIC FORAMINIFERA USING THE FORAMINIFERAL PRESERVATION INDEX: MAJOR IMPLICATIONS FOR GEOCHEMICAL PROXY RECORDS." In GSA 2020 Connects Online. Geological Society of America, 2020. http://dx.doi.org/10.1130/abs/2020am-350473.
Full textSheng, Qingyi. "MISSISSIPPIAN FORAMINIFERS FROM SOUTH CHINA." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-301287.
Full textReports on the topic "Foraminiferos"
Jennings, A. E., G. Vilks, B. Deonarine, A. Silis, and N. Weiner. Foraminiferal biostratigraphy and paleoceanography. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 2001. http://dx.doi.org/10.4095/212201.
Full textSilis, A. B. Late Quaternary foraminiferal biostratigraphy of Hudson Strait. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1993. http://dx.doi.org/10.4095/208321.
Full textHedinger, A. S. Distribution of Upper Jurassic foraminifers in the Beaufort-Mackenzie area. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207692.
Full textMcNeil, D. H., D. R. Issler, and L. R. Snowdon. Colour alteration, thermal maturity, and burial diagenesis in fossil foraminifers. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/208174.
Full textMcNeil, D. H. Distribution of Cenozoic agglutinated benthic foraminifers in the Beaufort-Mackenzie Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207695.
Full textMcNeil, D. H. Distribution of Cenozoic calcareous benthic foraminifers in the Beaufort-Mackenzie Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207696.
Full textPatterson, R. T. Neogene foraminiferal biostratigraphy of the southern Queen Charlotte Basin. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1989. http://dx.doi.org/10.4095/127725.
Full textMcNeil, D. H. Distribution of Albian to Maastrichtian benthic foraminifers in the Beaufort-Mackenzie area. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1996. http://dx.doi.org/10.4095/207694.
Full textHaggart, J. W., R. T. Patterson, and A. P. Dalby. Foraminifera from the Longarm Formation, Queen Charlotte Islands, British Columbia. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208599.
Full textThomas, F. C. The literature of Jurassic and early Cretaceous foraminifera - a compendium. Natural Resources Canada/ESS/Scientific and Technical Publishing Services, 1997. http://dx.doi.org/10.4095/208915.
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