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  • 1
    Buch
    Buch
    Amsterdam [u.a.] : Elsevier
    Schlagwort(e): Europa ; Paläoklima ; Miozän
    Materialart: Buch
    Seiten: 270 S. , Ill., graph. Darst., Kart.
    Serie: Palaeogeography, palaeoclimatology, palaeoecology 253.2007,1/2, Special issue
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 2
    Buch
    Buch
    Tübingen : Institut und Museum für Geologie und Paläontologie, Universität Tübingen
    Schlagwort(e): Dissertation ; Hochschulschrift ; Slowenien ; Ostalpen ; Oligozän ; Palynologie ; Paläoklima ; Palökologie ; Slowenien ; Ostalpen ; Oligozän ; Palynologie ; Paläoklima ; Palökologie
    Materialart: Buch
    Seiten: VI, 193, [80] S. , Ill., graph. Darst., Kt.
    Serie: Tuebinger mikropalaeontologische Mitteilungen 18
    RVK:
    Sprache: Deutsch
    Anmerkung: Literaturverz. S. 169 - 192 , Zugl.: Tübingen, Univ., Diss., 1998
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 3
    Schlagwort(e): Forschungsbericht ; Biodiversität ; Pflanzengeografie
    Materialart: Online-Ressource
    Seiten: 1 Online-Ressource (19 Seiten, 12,81 MB) , Illustrationen, Diagramme
    Sprache: Deutsch
    Anmerkung: Förderkennzeichen BMBF 01DK17023 , Verbundnummer 01179705 , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 4
    Publikationsdatum: 2023-03-08
    Schlagwort(e): Age, maximum/old; Age, minimum/young; Beibuwan_Depression; China; Coexistence Approach (Mosbrugger, V & Utescher, T, 1997); DRILL; Drilling/drill rig; Epoch; Event label; Fushan_Depression; Leizhou_Peninsula; Lühe; Lunpola_Basin; Markam; Miaoli; Namling; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; Ninghai; Number of taxa; Paleontological sampling; PALSAMP; Precipitation, annual mean, maximum; Precipitation, annual mean, minimum; Precipitation, warmest month, maximum; Precipitation, warmest month, minimum; Precipitation of the driest month maximum; Precipitation of the driest month minimum; Precipitation of the wettest month maximum; Precipitation of the wettest month minimum; Sample code/label; Shihti; South China Sea; Taiwan; Taxa analyzed; Temperature, annual mean, maximum; Temperature, annual mean, minimum; Temperature, coldest month, maximum; Temperature, coldest month, minimum; Temperature, warmest month, maximum; Temperature, warmest month, minimum; Tibet; Toupo_Basin; Weizhou_Island; Xianju; Xiaolongtan; Yinggehai_Depression; Zhujiangkou_Basin
    Materialart: Dataset
    Format: text/tab-separated-values, 806 data points
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 5
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    Unbekannt
    PANGAEA
    In:  Supplement to: Uhl, Dieter; Bruch, Angela A; Traiser, Christopher; Klotz, Stefan (2006): Palaeoclimate estimates for the Middle Miocene Schrotzburg flora (S Germany): a multi-method approach. International Journal of Earth Sciences, 95(6), 1071-1085, https://doi.org/10.1007/s00531-006-0083-9
    Publikationsdatum: 2023-05-12
    Beschreibung: We present a detailed palaeoclimate analysis of the Middle Miocene (uppermost Badenian-lowermost Sarmatian) Schrotzburg locality in S Germany, based on the fossil macro- and micro-flora, using four different methods for the estimation of palaeoclimate parameters: the coexistence approach (CA), leaf margin analysis (LMA), the Climate-Leaf Analysis Multivariate Program (CLAMP), as well as a recently developed multivariate leaf physiognomic approach based on an European calibration dataset (ELPA). Considering results of all methods used, the following palaeoclimate estimates seem to be most likely: mean annual temperature ~15-16°C (MAT), coldest month mean temperature ~7°C (CMMT), warmest month mean temperature between 25 and 26°C, and mean annual precipiation ~1,300 mm, although CMMT values may have been colder as indicated by the disappearance of the crocodile Diplocynodon and the temperature thresholds derived from modern alligators. For most palaeoclimatic parameters, estimates derived by CLAMP significantly differ from those derived by most other methods. With respect to the consistency of the results obtained by CA, LMA and ELPA, it is suggested that for the Schrotzburg locality CLAMP is probably less reliable than most other methods. A possible explanation may be attributed to the correlation between leaf physiognomy and climate as represented by the CLAMP calibration data set which is largely based on extant floras from N America and E Asia and which may be not suitable for application to the European Neogene. All physiognomic methods used here were affected by taphonomic biasses. Especially the number of taxa had a great influence on the reliability of the palaeoclimate estimates. Both multivariate leaf physiognomic approaches are less influenced by such biasses than the univariate LMA. In combination with previously published results from the European and Asian Neogene, our data suggest that during the Neogene in Eurasia CLAMP may produce temperature estimates, which are systematically too cold as compared to other evidence. This pattern, however, has to be further investigated using additional palaeofloras.
    Schlagwort(e): Germany, Baden-Wuerttemberg; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; OUTCROP; Outcrop sample; Schrotzburg
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 6
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    PANGAEA
    In:  Supplement to: Erdei, Boglarka; Hably, Lilla; Kazmer, Miklos; Utescher, Torsten; Bruch, Angela A (2007): Neogene flora and vegetation development of the Pannonian domain in relation to palaeoclimate and palaeogeography. Palaeogeography, Palaeoclimatology, Palaeoecology, 253(1-2), 131-156, https://doi.org/10.1016/j.palaeo.2007.03.036
    Publikationsdatum: 2023-05-12
    Beschreibung: A survey of the Neogene flora and vegetation pattern of the Pannonian domain based on 18 selected fossil plant assemblages is given. Flora and vegetation patterns are based on well-documented and studied fossil plant assemblages (macrofloras, primarily leaves). A general but slow cooling trend is definitely observable after the Early Miocene as reflected by both quantitative climate reconstructions and floristic change, i.e. decrease of diversity, slow disappearance of thermophilous and exotic elements, as well as decrease in the variety of vegetation types. A significant decline of coldest month temperatures (as compared to warmest month temperatures) must have played a defining role in forming flora and vegetation through the Neogene.
    Schlagwort(e): Andornaktalya; Budapest_city; Eger-Kiseged; Eger-Wind; Erdobenye-Barnamaj; Erdobenye-Kovago-oldal; Erdobenye-Ligetmajor; Felsotarkany; Gerce; Hungary; Hungary, Baranya; Hungary, Borsod-Abauj-Zemplen; Hungary, Budapest; Hungary, Fejer; Hungary, Heves; Hungary, Pest; Hungary, Vas; Hungary, Veszprem; Ipolytarnoc; Kesztolc; Magyaregregy; Nagybatony-Ujlak; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; Nogradszakal; OUTCROP; Outcrop sample; Pomaz; Pula; QU; Quarry; Tallya; Vertesszolos
    Materialart: Dataset
    Format: application/zip, 18 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 7
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    PANGAEA
    In:  Supplement to: Böhme, Madelaine; Bruch, Angela A; Selmeier, Alfred (2007): Implication of fossil wood for the reconstruction of Early and Middle Miocene climate and vegetation in the North Alpine Foreland Basin. Palaeogeography, Palaeoclimatology, Palaeoecology, 253(1-2), 107-130, https://doi.org/10.1016/j.palaeo.2007.03.035
    Publikationsdatum: 2023-01-14
    Beschreibung: Early- and Middle-Miocene sediments of the North Alpine Foreland Basin (NAFB) in Southern Germany contain one of the world richest regional records of silicified wood. Here we analyze over 1,000 identifiable samples, belonging to 80 wood anatomical taxa from 61 stratigraphically well-dated localities using principally the Coexistence Approach. The samples investigated originate from fluvial sediments representing periods of intensified surface runoff in the NAFB and therefore represent and provide information pertaining to the wet end-member of the fluctuating climate system. The dry end of the climate system is represented in the profiles either by hiatuses or palaeosoils. The dataset is split into four xylofloras: (I) the Ortenburg xyloflora (Late Ottnangian; ~17.5 to 17.3 Ma) originating from a paratropical evergreen Carapoxylon (Xylocarpus) forest; (II) the Southern Franconian Alb xyloflora (Late Karpatian; 17.0 to ~16.3 Ma) originating from a subtropical semideciduous limestone forest; (III) the upper Older Series xyloflora (Early Badenian; ~16.3 to ~15.3 Ma) originating from a subtropical oak-laurel forest; and (IV) the upper Middle Series xyloflora (Middle Badenian; 14.3 to ~13.8 Ma) originating from a subtropical dry deciduous forest.
    Schlagwort(e): Early Badenian; Germany, Bavaria; Late Karpatian; Late Ottnangian; Middle Badenian; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; North_Alpine_Foreland_1; North_Alpine_Foreland_2; North_Alpine_Foreland_3; North_Alpine_Foreland_4
    Materialart: Dataset
    Format: application/zip, 4 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 8
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    Unbekannt
    PANGAEA
    In:  Supplement to: Yao, Yi-Feng; Bruch, Angela A; Mosbrugger, Volker; Li, Cheng-Sen (2011): Quantitative reconstruction of Miocene climate patterns and evolution in Southern China based on plant fossils. Palaeogeography, Palaeoclimatology, Palaeoecology, 304(3-4), 291-307, https://doi.org/10.1016/j.palaeo.2010.04.012
    Publikationsdatum: 2023-01-13
    Beschreibung: Southern China, especially Yunnan, has undergone high tectonic activity caused by the uplift of Himalayan Mountains during the Neogene, which led to a fast changing palaeogeography. Previous study shows that Southern China has been influenced by the Asian Monsoon since at least the Early Miocene. However, it is yet not well understood how intense the Miocene monsoon system was. In the present study, 63 fossil floras of 16 localities from Southern China are compiled and evaluated for obtaining available information concerning floristic composition, stratigraphic age, sedimentology, etc. Based on such reliable information, selected mega- and micro-floras have been analysed with the coexistence approach to obtain quantitative palaeoclimate data. Visualization of climate results in maps shows a distinct spatial differentiation in Southern China during the Miocene. Higher seasonalities of temperature and precipitation occur in the north and south parts of Southern China, respectively. During the Miocene, most regions of Southern China and Europe were both warm and humid. Central Eurasia was likely to be an arid center, which gradually spread westward and eastward. Our data provide information about Miocene climate patterns in Southern China and about the evolution of these patterns throughout the Miocene, and is also crucial to unravel and understand the climatic signals of global cooling and tectonic uplift.
    Schlagwort(e): Beibuwan_Depression; China; DRILL; Drilling/drill rig; Fushan_Depression; Leizhou_Peninsula; Lühe; Lunpola_Basin; Markam; Miaoli; Namling; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; Ninghai; Paleontological sampling; PALSAMP; Shihti; South China Sea; Taiwan; Tibet; Toupo_Basin; Weizhou_Island; Xianju; Xiaolongtan; Yinggehai_Depression; Zhujiangkou_Basin
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 9
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    Unbekannt
    PANGAEA
    In:  Supplement to: Kern, Andrea; Harzhauser, Mathias; Mandic, Oleg; Roetzel, Reinhard; Coric, Stjepan; Bruch, Angela A; Zuschin, Martin (2011): Millennial-scale vegetation dynamics in an estuary at the onset of the Miocene Climate Optimum. Palaeogeography, Palaeoclimatology, Palaeoecology, 304(3-4), 247-261, https://doi.org/10.1016/j.palaeo.2010.07.014
    Publikationsdatum: 2023-01-13
    Beschreibung: Pollen analyses have been proven to possess the possibility to decipher rapid vegetational and climate shifts in Neogene sedimentary records. Herein, a c. 21-kyr-long transgression-regression cycle from the Lower Austrian locality Stetten is analysed in detail to evaluate climatic benchmarks for the early phase of the Middle Miocene Climate Optimum and to estimate the pace of environmental change. Based on the Coexistence Approach, a very clear signal of seasonality can be reconstructed. A warm and wet summer season with c. 204-236 mm precipitation during the wettest month was opposed by a rather dry winter season with precipitation of c. 9-24 mm during the driest month. The mean annual temperature ranged between 15.7 and 20.8 °C, with about 9.6-13.3 °C during the cold season and 24.7-27.9 °C during the warmest month. In contrast, today's climate of this area, with an annual temperature of 9.8 °C and 660 mm rainfall, is characterized by the winter season (mean temperature: -1.4 °C, mean precipitation: 39 mm) and a summer mean temperature of 19.9 °C (mean precipitation: 84 mm). Different modes of environmental shifts shaped the composition of the vegetation. Within few millennia, marshes and salt marshes with abundant Cyperaceae rapidly graded into Taxodiaceae swamps. This quick but gradual process was interrupted by swift marine ingressions which took place on a decadal to centennial scale. The transgression is accompanied by blooms of dinoflagellates and of the green alga Prasinophyta and an increase in Abies and Picea. Afterwards, the retreat of the sea and the progradation of estuarine and wetland settings were a gradual progress again. Despite a clear sedimentological cyclicity, which is related to the 21-kyr precessional forcing, the climate data show little variation. This missing pattern might be due to the buffering of the precessional-related climate signal by the subtropical vegetation. Another explanation could be the method-inherent broad range of climate-parameter estimates that could cover small scale climatic changes.
    Schlagwort(e): Austria; NECLIME; Neogene Climate Evolution in Eurasia; Paleontological sampling; PALSAMP; SPK-C; Stetten_section
    Materialart: Dataset
    Format: application/zip, 2 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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  • 10
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    PANGAEA
    In:  Supplement to: Syabryaj, Svetlana; Molchanoff, Serge; Utescher, Torsten; Bruch, Angela A (2007): Vegetation and palaeoclimate in the Miocene of Ukraine. Palaeogeography, Palaeoclimatology, Palaeoecology, 253(1-2), 169-184, https://doi.org/10.1016/j.palaeo.2007.03.038
    Publikationsdatum: 2023-01-14
    Beschreibung: Miocene deposits (marine and terrestrial) distributed throughout the whole territory of Ukraine contain numerous palaeontological remains including plant macro- and microfossils. The Miocene strata of Ukraine belong to the Central and the Eastern Paratethys and deposits from these regions have been studied palynologically. For the reconstruction of the vegetation of lowland and mountain areas in Ukraine palynological data have been complemented with data obtained from carpological and foliar studies. To obtain quantitative palaeoclimate data to reconstruct the Miocene climate evolution in the Carpathian realm and the Ukrainian Plain a total of 17 microfloral records combined from pollen counts of numerous samples are analyzed with respect to 7 climate variables using the Coexistence Approach.
    Schlagwort(e): Beregovo; Bolshie_Kopani; CDRILL; Chaplinka; Core drilling; Emetovka; Korobki; Leninskoe; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; Olkhovtsy; OUTCROP; Outcrop sample; Ternova; Ukraine, Khersonska; Ukraine, Krym; Ukraine, Odeska; Ukraine, Zakarpatska; Velikaya_Began; Voditsa; Zaluzh
    Materialart: Dataset
    Format: application/zip, 11 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
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