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Journal articles on the topic 'Rhaetian Alps'

Author: Grafiati

Published: 10 March 2023

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1

Senowbari-Daryan, Baba, and Michael Link. "Foraminifera from the Norian–Rhaetian reef carbonates of the Taurus Mountains (Saklıkent, Turkey)." Geologica Carpathica 68, no. 4 (2017): 303–17. http://dx.doi.org/10.1515/geoca-2017-0021.

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AbstractNorian–Rhaetian reef carbonates are exposed in several localities in Taurus Mountains. They predominately contain hypercalcified sponges, followed by scleractinian corals and other less numerous organisms. A coherent Norian–Rhaetian reef structure is exposed near the small town of Saklıkent, west of Antalya. Foraminifers occur in reef carbonates of Saklıkent by numerous genera as shown in this paper. Two species —Siculocosta tauricaandSiculocosta sadati— are described as new. The foraminiferal association of Saklıkent is similar or almost identical to the associations known from the No

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2

Senowbari-Daryan, B., and G. D. Stanley. "Taxonomic affinities and paleogeography of Stromatomorpha californica Smith, a distinctive Upper Triassic reef-adapted demosponge." Journal of Paleontology 83, no. 5 (2009): 783–93. http://dx.doi.org/10.1666/08-146.1.

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Stromatomorpha californica Smith is a massive, calcified, tropical to subtropical organism of the Late Triassic that produced small biostromes and contributed in building some reefs. It comes from the displaced terranes of Cordilleran North America (Eastern Klamath terrane, Alexander terrane, and Wrangellia). This shallow-water organism formed small laminar masses and sometimes patch reefs. It was first referred to the order Spongiomorphidae but was considered to be a coral. Other affinities that have been proposed include hydrozoan, stomatoporoid, sclerosponge, and chambered sponge. Part of t

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3

Schlagintweit, Felix, and Wolfgang Pavlik. "New findings of halimedacean algae from the Late Triassic Dachstein Limestone of the Northern Calcareous Alps (Hochschwab Area, Styria, Austria)." Geologia Croatica 61, no. 2-3 (2008): 129–33. http://dx.doi.org/10.4154/gc.2008.13.

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Two taxa of halimedacean algae are recorded from the Upper Triassic lagoonal Dachstein Limestone (Norian-Rhaetian) of the Hochschwab area in the south-eastern part of the Northern Calcareous Alps of Austria. They are described in open nomenclature as Halimeda? sp. 1 and Halimeda? sp. 2. In contrast to the widespread occurrence of dasycladacean algae, representatives of Halimedaceans are very rare. These findings are the second record in the Northern Calcareous Alps since FLÜGEL (1975).

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4

Gale, Luka, Bogomir Celarc, Marcello Caggiati, Tea Kolar-Jurkovšek, Bogdan Jurkovšek, and Piero Gianolla. "Paleogeographic significance of Upper Triassic basinal succession of the Tamar Valley, northern Julian Alps (Slovenia)." Geologica Carpathica 66, no. 4 (2015): 269–83. http://dx.doi.org/10.1515/geoca-2015-0025.

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AbstractThe Julian Alps (western Slovenia) structurally belong to the eastern Southern Alps. The Upper Triassic succession mostly consists of shallow water platform carbonates of the Dolomia Principale-Dachstein Limestone system and a deep water succession of the Slovenian Basin outcropping in the southern foothills of the Julian Alps. In addition to the Slovenian Basin, a few other intraplatform basins were present, but they remain poorly researched and virtually ignored in the existing paleogeographic reconstructions of the eastern Southern Alps. Herein, we describe a deepening-upward succes

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5

Gerdol, Renato, and Luca Bragazza. "Syntaxonomy and community ecology of mires in the Rhaetian Alps (Italy)." Phytocoenologia 31, no. 2 (2001): 271–99. http://dx.doi.org/10.1127/phyto/31/2001/271.

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6

Bechtel, Achim, Reinhard Gratzer, and Gerd Rantitsch. "Upper Triassic (Rhaetian) mudstones (Kössen Formation) within the central Gailtal Alps (Eastern Alps, Austria) as potential hydrocarbon source rocks." Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen 222, no. 3 (2001): 427–51. http://dx.doi.org/10.1127/njgpa/222/2001/427.

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7

Granzow, Wolfgang. "Two new problematic microfossils from Norian and Rhaetian of the Allgäu-Alps." Neues Jahrbuch für Geologie und Paläontologie - Monatshefte 1989, no. 2 (1989): 65–78. http://dx.doi.org/10.1127/njgpm/1989/1989/65.

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8

Muttoni, Giovanni, Dennis V. Kent, Flavio Jadoul, et al. "Rhaetian magneto-biostratigraphy from the Southern Alps (Italy): Constraints on Triassic chronology." Palaeogeography, Palaeoclimatology, Palaeoecology 285, no. 1-2 (2010): 1–16. http://dx.doi.org/10.1016/j.palaeo.2009.10.014.

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9

Gale, Luka, Tea Kolar-Jurkovšek, Andrej Šmuc, and Boštjan Rožič. "Integrated Rhaetian foraminiferal and conodont biostratigraphy from the Slovenian Basin, eastern Southern Alps." Swiss Journal of Geosciences 105, no. 3 (2012): 435–62. http://dx.doi.org/10.1007/s00015-012-0117-1.

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10

Scapozza, Cristian, Chantal Del Siro, Christophe Lambiel, and Christian Ambrosi. "Schmidt hammer exposure-age dating of periglacial and glacial landforms in the Southern Swiss Alps based on <i>R</i>-value calibration using historical data." Geographica Helvetica 76, no. 4 (2021): 401–23. http://dx.doi.org/10.5194/gh-76-401-2021.

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Abstract. As a contribution to the palaeoenvironmental history reconstruction of the Alpine periglacial domain, this study focuses on the Schmidt hammer exposure-age dating (SHD) of (peri-)glacial landforms using rebound-value (R-value) calibrations for 10 stations in the Scaradra glacier forefield (north-eastern part of the Ticino Canton, Lepontine Alps) and for 13 stations in the Splügenpass region (located between Switzerland and Italy, Rhaetian Alps). Linear calibration based on the known age of several moraines of the Scaradra glacier assessed by historical cartography allowed the reconst

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11

Schlagintweit, Felix, Sigrid Missoni, and Hans-Juergen Gawlick. "Coptocampylodon? rhaeticus n.sp., a New Problematic Microfossil (“incertae sedis”) from the Rhaetian Dachstein Limestone of the Northern Calcareous Alps (Germany, Austria)." Geologia Croatica 55, no. 2 (2002): 107–19. http://dx.doi.org/10.4154/gc.2002.12.

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A new problematic microfossil is described as Coptocampylodon? rhaeticus n.sp. from the Rhaetian Dachstein Limestone of the Northern Calcareous Alps. The new species is composed of a long cylindrical and an irregular rounded body, both showing narrow axial cavity. It is similar to Coptocampylodon? elliotti RADOIČIĆ 1969 from the Cenomanian of Montenegro, but lacks the longitudinal grooves in the cylindrical part. In the Alpine Dachstein Limestone it has been detected at several localities where it occurs as an abundant constituent of biosparitic limestones along with the benthic foraminifera T

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12

Lakew, Tesfaye. "Microfacies and cyclic sedimentation of the Upper Triassic (Rhaetian) Calcare di zu (Southern Alps)." Facies 22, no. 1 (1990): 187–231. http://dx.doi.org/10.1007/bf02536952.

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13

Smiraglia, C. "The Medial Moraines of Ghiacciaio Dei Forni, Valtellina, Italy: Morphology and Sedimentology." Journal of Glaciology 35, no. 119 (1989): 81–84. http://dx.doi.org/10.3189/002214389793701428.

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AbstractTwo distinct medial moraines are located on the tongue of Ghiacciaio dei Forni (Rhaetian Alps, Italy); they are formed by the confluence of three ice streams. The two ice-cored medial moraines originate from rock outcrops situated below the snow line. The moraines, which on the surface comprise angular clasts, extend for approximately 2 km and reach a maximum height of 10 m. Nourishment of the moraines seems to be due primarily to the supraglacial debris derived from the rock walls. Measurements made in the late summer of 1985 provided evidence of the role played by differential ablati

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14

Gale, Luka. "Rhaetian foraminiferal assemblage from the Dachstein Limestone of Mt. Begunjščica (Košuta Unit, eastern Southern Alps)." Geologija 55, no. 1 (2012): 17–44. http://dx.doi.org/10.5474/geologija.2012.002.

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15

Oprčkal, Primož, Luka Gale, Tea Kolar-Jurkovšek, and Boštjan Rožič. "Outcrop-scale evidence for the Norian-Rhaetian extensional tectonics in the Slovenian Basin (Southern Alps)." Geologija 55, no. 1 (2012): 45–56. http://dx.doi.org/10.5474/geologija.2012.003.

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16

Boštjan, Rožič, Gale Luka, and Kolar-Jurkovšek Tea. "Extent of the Upper Norian – Rhaetian Slatnik Formation in the Tolmin Nappe, eastern Southern Alps." Geologija 56, no. 2 (2013): 175–86. http://dx.doi.org/10.5474/geologija.2013.011.

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17

Kristan-Tollmann, Edith, and Vishwa J. Gupta. "Identidy of the lower Rhaetian microfauna of the Zlambach- and Kioto Marls (Eastern Alps - Himalaya)." Newsletters on Stratigraphy 20, no. 1 (1988): 1–6. http://dx.doi.org/10.1127/nos/20/1988/1.

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18

Leary, T. J. "Martial 14.100: Panaca." Classical Quarterly 47, no. 1 (1997): 322–23. http://dx.doi.org/10.1093/cq/47.1.322.

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The wine referred to in the second line of the epigram was produced near Verona, at the foot of the Rhaetian Alps. It was well regarded by most and was a favourite of the Emperor Augustus: for references see Mynors at Verg. G. 2.96 and my note at Mart. 14.100.2. It appears, however, to have undue prominence in this poem, supposedly about the earthenware drinking vessels which, presumably, were manufactured in the same area.There is also the question of why Martial refers to Verona in such a circumlocutory way. Is he merely following a well established elegiac/epigrammatic convention in associa

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19

Demangel, Isaline, Zsófia Kovács, Silvia Gardin, et al. "Fate of calcareous nannofossils during the Rhaetian (Late Triassic): evidence from the Northern Calcareous Alps, Austria." Lethaia 56, no. 1 (2023): 1–24. http://dx.doi.org/10.18261/let.56.1.5.

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20

Golzio, Alessio, Silvia Ferrarese, Claudio Cassardo, Gugliemina Adele Diolaiuti, and Manuela Pelfini. "Land-Use Improvements in the Weather Research and Forecasting Model over Complex Mountainous Terrain and Comparison of Different Grid Sizes." Boundary-Layer Meteorology 180, no. 2 (2021): 319–51. http://dx.doi.org/10.1007/s10546-021-00617-1.

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AbstractWeather forecasts over mountainous terrain are challenging due to the complex topography that is necessarily smoothed by actual local-area models. As complex mountainous territories represent 20% of the Earth’s surface, accurate forecasts and the numerical resolution of the interaction between the surface and the atmospheric boundary layer are crucial. We present an assessment of the Weather Research and Forecasting model with two different grid spacings (1 km and 0.5 km), using two topography datasets (NASA Shuttle Radar Topography Mission and Global Multi-resolution Terrain Elevation

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21

Baroni, Carlo, Stefano Casale, Maria Cristina Salvatore, et al. "Double response of glaciers in the Upper Peio Valley (Rhaetian Alps, Italy) to the Younger Dryas climatic deterioration." Boreas 46, no. 4 (2017): 783–98. http://dx.doi.org/10.1111/bor.12284.

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22

Pecetti, L., M. Romani, P. Spoleto, A. Tosca, G. Della Marianna, and F. Gusmeroli. "Morpho-physiological variation ofPoa alpinaL. genetic resources from the Rhaetian Alps, Italy, grown in two altitude-contrasting sites." Grass and Forage Science 70, no. 3 (2014): 530–37. http://dx.doi.org/10.1111/gfs.12140.

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23

Mette, Wolfgang, Armin Elsler, and Christoph Korte. "Palaeoenvironmental changes in the Late Triassic (Rhaetian) of the Northern Calcareous Alps: Clues from stable isotopes and microfossils." Palaeogeography, Palaeoclimatology, Palaeoecology 350-352 (September 2012): 62–72. http://dx.doi.org/10.1016/j.palaeo.2012.06.013.

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24

Pecetti, Luciano, Aldo Tava, Massimo Romani, Roberto Cecotti, and Mariella Mella. "Variation in Terpene and Linear-Chain Hydrocarbon Content in Yarrow (Achillea millefoliumL.) Germplasm from the Rhaetian Alps, Italy." Chemistry & Biodiversity 9, no. 10 (2012): 2282–94. http://dx.doi.org/10.1002/cbdv.201200072.

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25

Baroni, Carlo, Salvatore Martino, Maria Cristina Salvatore, Gabriele Scarascia Mugnozza, and Luca Schilirò. "Thermomechanical stress–strain numerical modelling of deglaciation since the Last Glacial Maximum in the Adamello Group (Rhaetian Alps, Italy)." Geomorphology 226 (December 2014): 278–99. http://dx.doi.org/10.1016/j.geomorph.2014.08.013.

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26

Cerrato, Riccardo, Maria Cristina Salvatore, Björn E. Gunnarson, et al. "A Pinus cembra L. tree-ring record for late spring to late summer temperature in the Rhaetian Alps, Italy." Dendrochronologia 53 (February 2019): 22–31. http://dx.doi.org/10.1016/j.dendro.2018.10.010.

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27

Gale, Luka. "Microfacies analysis of the Upper Triassic (Norian) "Bača Dolomite": early evolution of the western Slovenian Basin (eastern Southern Alps, western Slovenia)." Geologica Carpathica 61, no. 4 (2010): 293–308. http://dx.doi.org/10.2478/v10096-010-0017-0.

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Microfacies analysis of the Upper Triassic (Norian) "Bača Dolomite": early evolution of the western Slovenian Basin (eastern Southern Alps, western Slovenia)The Slovenian Basin represents a Mesozoic deep-water sedimentary environment, situated on the southern Tethyan passive margin. Little is known about its earliest history, from the initial opening in the Carnian (probably Ladinian) to a marked deepening at the beginning of the Jurassic. The bulk of the sediment deposited during this period is represented by the Norian-Rhaetian "Bača Dolomite", which has, until now, been poorly investigated

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28

Cerrato, Riccardo, Maria Cristina Salvatore, Björn E. Gunnarson, et al. "Pinus cembra L. tree-ring data as a proxy for summer mass-balance variability of the Careser Glacier (Italian Rhaetian Alps)." Journal of Glaciology 66, no. 259 (2020): 714–26. http://dx.doi.org/10.1017/jog.2020.40.

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AbstractGlacial extent and mass balance are sensitive climate proxies providing solid information on past climatic conditions. However, series of annual mass-balance measurements of more than 60 years are scarce. To our knowledge, this is the first time the latewood density data (MXD) of the Swiss stone pine (Pinus cembra L.) have been used to reconstruct the summer mass balance (Bs) of an Alpine glacier. The MXD-based Bs well correlates with a Bs reconstruction based on the May to September temperature. Winter precipitation has been used as an independent proxy to infer the winter mass balanc

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29

McROBERTS, CHRISTOPHER A., LEOPOLD KRYSTYN, and ADRIEL SHEA. "RHAETIAN (LATE TRIASSIC) MONOTIS (BIVALVIA: PECTINOIDA) FROM THE EASTERN NORTHERN CALCAREOUS ALPS (AUSTRIA) AND THE END-NORIAN CRISIS IN PELAGIC FAUNAS." Palaeontology 51, no. 3 (2008): 721–35. http://dx.doi.org/10.1111/j.1475-4983.2008.00776.x.

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30

HAUFFE, H. "Evolution of the chromosomal races ofMus musculus domesticusin the Rhaetian Alps: the roles of whole-arm reciprocal translocation and zonal raciation." Biological Journal of the Linnean Society 62, no. 2 (1997): 255–78. http://dx.doi.org/10.1006/bijl.1997.0153.

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31

Mette, Wolfgang, Marie-Emilie Clemence, Nicolas Thibault, Christoph Korte, Bernadette Konrad, and Clemens Vinzenz Ullmann. "Sedimentology, carbon isotope stratigraphy and micropalaeontology of the Rhaetian Zlambach Formation– Implications for the Dachstein carbonate platform development (Northern Calcareous Alps, Austria)." Sedimentary Geology 382 (March 2019): 47–60. http://dx.doi.org/10.1016/j.sedgeo.2018.12.009.

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32

Pecetti, L., M. Romani, L. De Rosa, et al. "Variation in morphology and seed production of snow clover [Trifolium pratense L. subsp. nivale (Koch) Arcang.] germplasm from the Rhaetian Alps, Italy." Genetic Resources and Crop Evolution 55, no. 7 (2007): 939–47. http://dx.doi.org/10.1007/s10722-007-9301-y.

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33

Hauffe, Heidi C., and Jaroslav Piálek. "Evolution of the chromosomal races of Mus musculus domesticus in the Rhaetian Alps: the roles of whole-arm reciprocal translocation and zonal raciation." Biological Journal of the Linnean Society 62, no. 2 (1997): 255–78. http://dx.doi.org/10.1111/j.1095-8312.1997.tb01626.x.

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34

Sasvari, Agoston, Laura Davies, Andrew Mann, Jawad Afzal, Gabor Vakarcs, and Eugene Iwaniw. "Dachstein-type Avroman Formation: An indicator of the Harsin Basin in Iraq." GeoArabia 20, no. 4 (2015): 17–36. http://dx.doi.org/10.2113/geoarabia200417.

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ABSTRACT A field survey was carried out in 2012 focusing on the tectonic position and the role of Upper Triassic (Upper Norian–Rhaetian) Avroman Formation outcrops located in the Zalm area of Iraq, close to the Iraq-Iran border. At this location, the Cretaceous chert-bearing strata of the Qulqula Formation are overlain by sheared mafic bodies, which are in turn topped by the cliffs of the megalodontaceae-bearing Upper Triassic Avroman Formation. Similarities in lithology, sequence and tectonics position, suggest that the Triassic section of the Bisotoun Unit from the Kermanshah Zone of Iran ca

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35

Pecetti, Luciano, Massimo Romani, Paola Spoleto, Alberto Tosca, Gianpaolo Della Marianna, and Fausto Gusmeroli. "Effect of Geographic Origin and Ex Situ Growing Site on Phenology, Morphology, and Seed Yield of Yarrow (Achillea millefoliumL.) Germplasm from the Rhaetian Alps, Italy." Restoration Ecology 22, no. 4 (2014): 502–8. http://dx.doi.org/10.1111/rec.12099.

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36

Ochyra, Ryszard. "Bryoerythrophyllum alpigenum (Bryophyta, Pottiaceae) confirmed in the moss flora of Poland, with a review of the nomenclatural issues associated with this species name." Folia Cryptogamica Estonica 58 (October 20, 2020): 1–17. http://dx.doi.org/10.12697/fce.2021.58.01.

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   Occurrence of Bryoerythrophyllum alpigenum (Jur.) P.C.Chen in Poland is confirmed. The species is known from a single record from the Western Tatra Mountains in the Polish Western Carpathians. A description and illustrations of the Polish material of this species is provided and its distribution mapped. Taxonomic and nomenclatural comments on B. alpigenum are presented and its global geographical distribution is reviewed. This species was first recognised as a variety, Didymodon rubellus var. dentatus Schimp., in 1860 by W. P. Schimper. It was subsequently described in 188

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37

Belloni, V., D. Fugazza, and M. Di Rita. "UAV-BASED GLACIER MONITORING: GNSS KINEMATIC TRACK POST-PROCESSING AND DIRECT GEOREFERENCING FOR ACCURATE RECONSTRUCTIONS IN CHALLENGING ENVIRONMENTS." International Archives of the Photogrammetry, Remote Sensing and Spatial Information Sciences XLIII-B1-2022 (May 30, 2022): 367–73. http://dx.doi.org/10.5194/isprs-archives-xliii-b1-2022-367-2022.

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Abstract. Continuous monitoring of glaciers is of key importance to understand their morphological evolution over time and monitor the impact of climate change. Recently, Unmanned Aerial Vehicles (UAVs) have proven to be ideal candidates for glacier monitoring thanks to their flexibility and ease of processing with software packages. Traditionally, for high-accurate and geodetically relevant results, Ground Control Points (GCPs) need to be homogeneously distributed over the area of interest and manually identified in the imagery to guarantee accurate reconstructions. However, the GCP setup is

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38

Goričan, Špela, Martin Đaković, Peter O. Baumgartner, et al. "Mesozoic basins on the Adriatic continental margin – a cross-section through the Dinarides in Montenegro / Mezozojski bazeni na kontinentalnem robu Jadranske plošče – presek čez Dinaride v Črni gori." Folia biologica et geologica 63, no. 2 (2022): 85–150. http://dx.doi.org/10.3986/fbg0099.

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The Dinarides, together with the Albanides and Hellenides, preserve stratigraphic successions derived from the eastern margin of the Adriatic microplate and remnants of ophiolites obducted from the Maliac-Vardar branch of the Neotethys Ocean. The main stages in the Mesozoic geodynamic history are: 1) rifting leading to opening of the Maliac Ocean in the Late Anisian, 2) onset of an east-dipping intra-oceanic subduction in the Early-Middle Jurassic and sea-floor spreading in a supra-subduction setting (Vardar Ocean), 3) formation of ophiolitic mélanges in trench-like basins, westward obduction

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39

Nützel, Alexander, Martin Nose, Michael Hautmann, and Rupert Hochleitner. "Latest Triassic (Sevatian–Rhaetian) reef carbonates from the Northern Calcareous Alps (Austria), their mollusc dwellers, and their fate at the end-Triassic extinction event." PalZ, December 9, 2022. http://dx.doi.org/10.1007/s12542-022-00631-9.

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AbstractA reef-associated mollusc fauna (gastropods and bivalves) and its facies context are described from latest Triassic (Sevatian–Rhaetian) reef carbonates of Austria (Rötelwand reef at Gaissau and Gosaukamm near Hallstatt). The studied carbonates from the Rötelwand reef consist of mollusc-rich rudstones, partly boundstones, which contain branched corals (Cycliphyllia and Retiophylia, Pinacophyllum), whereas coralline sponges are absent. The rich foraminiferid fauna that is associated with the reef builders consists of 11 genera; eight of these genera became extinct until the end of the Rh

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40

Larina, Ekaterina, Sylvain Richoz, Niklas Hohmann, Emilia Jarochowska, David Bottjer, and Frank Corsetti. "Microfacies and Macrofaunal Analysis of Upper Rhaetian Eibergmember Sequences from the Northern Calcareous Alps." SSRN Electronic Journal, 2022. http://dx.doi.org/10.2139/ssrn.4264473.

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41

Boggero, Angela, Silvia Zaupa, Simona Musazzi, Michela Rogora, Elzbieta Dumnicka, and Andrea Lami. "Environmental factors as drivers for macroinvertebrate and diatom diversity in Alpine lakes: New insights from the Stelvio National Park (Italy)." Journal of Limnology 78, no. 2 (2019). http://dx.doi.org/10.4081/jlimnol.2019.1863.

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Information on the biodiversity of high altitude lakes in the Stelvio National Park was scarce and fragmentary, in most cases limited to a few studies on a single biological issue. To fill this gap, a multidisciplinary research program was established in 2011 to investigate macroinvertebrates, diatoms, and water chemistry in 8 high altitude lakes within the boundaries of the Park (Rhaetian Alps, Eastern Alps). The results of this study were compared with data on biological assemblages and chemical parameters of Alpine lakes in the Pennine-Lepontine Alps (Western Alps), to evaluate the role of

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42

Scheyer, Torsten M., Urs Oberli, Nicole Klein, and Heinz Furrer. "A large osteoderm-bearing rib from the Upper Triassic Kössen Formation (Norian/Rhaetian) of eastern Switzerland." Swiss Journal of Palaeontology 141, no. 1 (2022). http://dx.doi.org/10.1186/s13358-022-00244-4.

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AbstractAn important component of the Alpine vertebrate record of Late Triassic age derives from the Kössen Formation, which crops out extensively in the eastern Alps. Here, we present an isolated and only partially preserved large rib, which carries an osteoderm on a low uncinate process. Osteological comparison indicates that the specimen likely belongs to a small clade of marine reptiles, Saurosphargidae. Members of the clade are restricted to the western (today Europe) and eastern margins of the Tethys (today China) and were so far known only from the Anisian stage of the Middle Triassic.

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