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  • 1
    Monograph available for loan
    Monograph available for loan
    Kyoto : International Research Center for Japanese Studies
    Associated volumes
    Call number: AWI Bio-18-91448
    In: The pollen flora of Yunnan, China, Vol. 1
    Description / Table of Contents: The Pollen Flora of Yunnan, China is the first book of the series of pollen morphological studies of tree plants growing in the wild in the Yunnan Province and in the surrounding area of China: Asian Environmental History. The series will present the first detailed work on the pollen flora of China. This book includes electron microscope photographs and light micrographs of 67 species of Gymnosperm, Myricaceae and Juglandaceae and can be used for research on many areas including pollen analysis and plant taxonomy.
    Type of Medium: Monograph available for loan
    Pages: 144 S.
    ISBN: 8174363416
    Series Statement: Asian Environmental History 1
    Language: English
    Note: Contents: Preface. - Introduction. - Gymnosperm. - Pinaceae. - Taxodiaceae. - Cupressaceae. - Podocarpaceae. - Ephedraceae. - Angiosperm. - Juglandaceae. - Myricaceae. - Bibliography. - Plates. - Gymnosperm. - Pinaceae: Plates 1-23. - Taxodiaceae: Plates 24-26. - Cupressaceae: Plates 27-39. - Podocarpaceae: Plates 40-46. - Ephedraceae: Plates 47-52. - Angiosperm. - Juglandaceae: Plates 53-64. - Myricaceae: Plates 64-68. - Pollen Sample List. - Index.
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
    Publication Date: 2023-03-08
    Keywords: Age, maximum/old; Age, minimum/young; Bohai_Gulf_Basin; Bozhong; China; Coexistence Approach (Mosbrugger, V & Utescher, T, 1997); Dunhua; Dunhuang; Epoch; Erlian_Basin; Event label; Huanan; Huanghua; Hunchun; Jidong; Jiyang_Bozhong_Basins; Kuqa; Lantian; Mongolia; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; 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; Sample type; Shangdou_Huade_Basin; Shanwang; Southern_Junggar_Basin; Temperature, annual mean, maximum; Temperature, annual mean, minimum; Temperature, coldest month, maximum; Temperature, coldest month, minimum; Temperature, warmest month, maximum; Temperature, warmest month, minimum; Tianchang; Wulougong; Xining_Minhe_Basin; Zhoukou_Basin
    Type: Dataset
    Format: text/tab-separated-values, 664 data points
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Jacques, Frédéric M B; Guo, Shuang-Xing; Su, Tao; Xing, Yao-Wu; Huang, Yong-Jiang; Liu, Yu-Sheng Christopher; Ferguson, David-Kay; Zhou, Zhekun (2011): Quantitative reconstruction of the Late Miocene monsoon climates of southwest China: A case study of the Lincang flora from Yunnan Province. Palaeogeography, Palaeoclimatology, Palaeoecology, 304(3-4), 318-327, https://doi.org/10.1016/j.palaeo.2010.04.014
    Publication Date: 2024-02-17
    Description: The Miocene Lincang leaf assemblage is used in this paper as proxy data to reconstruct the palaeoclimate of southwestern Yunnan (SW China) and the evolution of monsoon intensity. Three quantitative methods were chosen for this reconstruction, i.e. Leaf Margin Analysis (LMA), Climate Leaf Analysis Multivariate Program (CLAMP), and the Coexistence Approach (CA). These methods, however, yield inconsistent results, particularly for the precipitation, as also shown in European and other East Asian Cenozoic floras. The wide range of the reconstructed climatic parameters includes the Mean Annual Temperature (MAT) of 18.5-24.7 °C and the Mean Annual Precipitation (MAP) of 1213-3711 mm. Compared with the modern Lincang climate (MAT, 17.3 °C; MAP, 1178.7 mm), the Miocene climate is slightly warmer, wetter and has a higher temperature seasonality. A detailed comparison on the palaeoclimatic variables with the coeval Late Miocene Xiaolongtan flora from the eastern part of Yunnan allows us to investigate the development and interactions of both South Asian and East Asian monsoons during the Late Miocene in southwest China, now under strong influence of these monsoon systems. Our results suggest that the monsoon climate has already been established in southwest Yunnan during the Late Miocene. Furthermore, our results support that both Southeast Asian and East Asian monsoons co-occurred in Yunnan during the Late Miocene.
    Keywords: Lincang; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; Paleontological sampling; PALSAMP; Yunnan, China
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Xing, Yao-Wu; Utescher, Torsten; Jacques, Frédéric M B; Su, Tao; Liu, Yu-Sheng Christopher; Huang, Yong-Jiang; Zhou, Zhekun (2012): Palaeoclimatic estimation reveals a weak winter monsoon in southwestern China during the late Miocene: Evidence from plant macrofossils. Palaeogeography, Palaeoclimatology, Palaeoecology, 358-360, 19-26, https://doi.org/10.1016/j.palaeo.2012.07.011
    Publication Date: 2024-02-17
    Description: The late Miocene Xianfeng flora of Yunnan Province, southwestern China, was chosen to reconstruct the paleoclimate and the intensity of the Asian monsoon. Three available quantitative climate reconstruction methods from fossil plants, i.e. Leaf Margin Analysis (LMA), the Climate Leaf Analysis Multivariate Program (CLAMP), and the Coexistence Approach (CA) were used in this study. MATs (mean annual temperatures) resulting from these three approaches (i.e., LMA: 17.2 ± 2.38 °C; CLAMP: 15.43 ± 1.25 °C; CA: 17.2-21.7 °C) appear to have been higher than the present (14.9 °C), suggesting a much warmer climate in the late Miocene. Both the growing season precipitation (GSP) from CLAMP (1908.7 ± 217.7 mm) and mean annual precipitation (MAP) from CA (1206.0-1613.0 mm) estimates are higher than modern values (1003.2 mm (GSP) and 1038 mm (MAP) respectively) indicating a more humid climate during the late Miocene. By comparing these with climates reconstructed from neighboring late Miocene floras, we conclude that the general late Miocene climate appears warmer and more humid than present conditions in southwestern China. Furthermore, the evident differences in estimated monthly temperatures between the summer and winter, and precipitations between the humid and dry seasons indicate the existence of seasonality, though not as strong as that of today. Difference in precipitation of dry season indicates a marked strengthening in the winter monsoon since the late Miocene. A new monsoon intensity index has also been defined based on precipitation seasonality to investigate the intensity of the Asian monsoon.
    Keywords: Yunnan_Province; Yunnan, China
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 5
    Publication Date: 2024-02-17
    Keywords: Climate-Leaf Analysis Multivariate Program (CLAMP) (Wolfe, 1993); Leaf apex attenuate; Leaf apex emarginate; Leaf apex round; Leaf base acute; Leaf base cordate; Leaf base round; Leaf length/width ratio 〈 1:1; Leaf length/width ratio 〉 4:1; Leaf length/width ratio 1-2:1; Leaf length/width ratio 2-3:1; Leaf length/width ratio 3-4:1; Leaf lobed; Leaf margin, entire; Leaf margin teeth acute; Leaf margin teeth close; Leaf margin teeth compound; Leaf margin teeth regular; Leaf margin teeth round; Leaf shape ellipitic; Leaf shape obovate; Leaf shape ovate; Leaf size leptophyll 1, 5-20 mm2; Leaf size leptophyll 2, 20-80 mm2; Leaf size mesophyll 1, 3600-6200 mm2; Leaf size mesophyll 2, 6200-10000 mm2; Leaf size mesophyll 3, 〉 10000 mm**2; Leaf size microphyll 1, 80-400 mm2; Leaf size microphyll 2, 400-1400 mm2; Leaf size microphyll 3, 1400-3600 mm2; Leaf size nanophyll, 〈 5 mm**2; Lincang; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; Paleontological sampling; PALSAMP; Yunnan, China
    Type: Dataset
    Format: text/tab-separated-values, 31 data points
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  • 6
    Publication Date: 2024-02-17
    Keywords: Climate-Leaf Analysis Multivariate Program (CLAMP) (Wolfe, 1993); Leaf apex acute; Leaf apex attenuate; Leaf apex emarginate; Leaf apex round; Leaf base acute; Leaf base cordate; Leaf base round; Leaf length/width ratio 〈 1:1; Leaf length/width ratio 〉 4:1; Leaf length/width ratio 1-2:1; Leaf length/width ratio 2-3:1; Leaf length/width ratio 3-4:1; Leaf lobed; Leaf margin entire (no teeth); Leaf margin teeth; Leaf margin teeth acute; Leaf margin teeth close; Leaf margin teeth compound; Leaf margin teeth distant; Leaf margin teeth irregular; Leaf margin teeth regular; Leaf margin teeth round; Leaf shape ellipitic; Leaf shape obovate; Leaf shape ovate; Leaf size leptophyll 1, 5-20 mm**2; Leaf size leptophyll 2, 20-80 mm**2; Leaf size mesophyll 1, 3600-6200 mm**2; Leaf size mesophyll 2, 6200-10000 mm**2; Leaf size mesophyll 3, 〉 10000 mm**2; Leaf size microphyll 1, 80-400 mm**2; Leaf size microphyll 2, 400-1400 mm**2; Leaf size microphyll 3, 1400-3600 mm**2; Leaf size nanophyll, 〈 5 mm**2; Leaf unlobed; ORDINAL NUMBER; Species; Yunnan_Province; Yunnan, China
    Type: Dataset
    Format: text/tab-separated-values, 1998 data points
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  • 7
    Publication Date: 2024-02-17
    Keywords: 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; Species; Taxon/taxa; Temperature, annual mean, maximum; Temperature, annual mean, minimum; Temperature, coldest month, maximum; Temperature, coldest month, minimum; Temperature, warmest month, maximum; Temperature, warmest month, minimum; Yunnan_Province; Yunnan, China
    Type: Dataset
    Format: text/tab-separated-values, 528 data points
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  • 8
    Publication Date: 2024-02-17
    Keywords: Age, maximum/old; Age, minimum/young; Climate-Leaf Analysis Multivariate Program (CLAMP) (Wolfe, 1993); Coexistence Approach (Mosbrugger, V & Utescher, T, 1997); Enthalpy; Epoch; Formation; Growing season length; Humidity, relative; Humidity, specific; Lincang; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; Paleontological sampling; PALSAMP; Precipitation, annual mean, maximum; Precipitation, annual mean, minimum; Precipitation, growing season; Precipitation, monthly mean growing season; Precipitation, warmest month, maximum; Precipitation, warmest month, minimum; Precipitation of 3 consecutive driest months per year; Precipitation of 3 consecutive wettest months per year; 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 comment; Taxa analyzed; Temperature, annual mean; Temperature, annual mean, maximum; Temperature, annual mean, minimum; Temperature, coldest month; Temperature, coldest month, maximum; Temperature, coldest month, minimum; Temperature, warmest month; Temperature, warmest month, maximum; Temperature, warmest month, minimum; Yunnan, China
    Type: Dataset
    Format: text/tab-separated-values, 37 data points
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  • 9
    Publication Date: 2024-02-17
    Keywords: Age, maximum/old; Age, minimum/young; Albizia sp.; Aphanamixis sp.; Berchemia sp.; Betula mioluminifera; Bumelia pseudolycioides; Calocedrus lantenoisi; Capparis sp.; Castanopsis sp.; Celtis miobungeana; Chrysophyllum sp.; Cinnamomum naitoanum; Cinnamomum scheuchzeri; Cinnamomum sp.; Cyclobalanopsis mandraliscae; Cyclobalanopsis sp.; Dalbergia prehupeana; Desmodium sp.; Engelhardia sp.; Epoch; Ficus sp.; Formation; Fossil determination; Gleditsia miosinensis; Glyptostrobus europaeus; Helicteres sp.; Hydrangea lanceolimba; Ilex sp.; Koelreuteria sp.; Lincang; Lithocarpus reniifolius; Lithocarpus sp.; Litsea grabaui; Loranthus palaeoeuropaeus; Lumnitzera sp.; Maackia sp.; Milletia sp.; Mucuna sp.; Murraya sp.; NECLIME; NECLIME_campaign; Neocinnamomum sp.; Neogene Climate Evolution in Eurasia; Ormosia sp.; Paleontological sampling; PALSAMP; Photinia sp.; Piper sp.; Pistacia miochinensis; Pittosporum sp.; Populus glandulifera; Quercus latifolia; Quercus simulata; Quercus sp.; Reevesia sp.; Rhus sp.; Schisandra sp.; Schoepfia sp.; Sediment type; Shuteria sp.; Smilax grandifolia; Sorbus sp.; Stranvaesia sp.; Styrax sp.; Syzygium sp.; Terminalia sp.; Ternstroemia maekawai; Tetragonia sp.; Toona bienensis; Toxicodendron sp.; Viburnum sp.; Yunnan, China; Zanthoxylum sp.
    Type: Dataset
    Format: text/tab-separated-values, 66 data points
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  • 10
    Publication Date: 2024-02-17
    Keywords: Climate-Leaf Analysis Multivariate Program (CLAMP) (Wolfe, 1993); Fossil determination; Leaf apex acute; Leaf apex attenuate; Leaf apex emarginate; Leaf apex round; Leaf base acute; Leaf base cordate; Leaf base round; Leaf length/width ratio 〈 1:1; Leaf length/width ratio 〉 4:1; Leaf length/width ratio 1-2:1; Leaf length/width ratio 2-3:1; Leaf length/width ratio 3-4:1; Leaf lobed; Leaf margin entire (no teeth); Leaf margin teeth acute; Leaf margin teeth close; Leaf margin teeth compound; Leaf margin teeth regular; Leaf margin teeth round; Leaf shape ellipitic; Leaf shape obovate; Leaf shape ovate; Leaf size leptophyll 1, 5-20 mm**2; Leaf size leptophyll 2, 20-80 mm**2; Leaf size mesophyll 1, 3600-6200 mm**2; Leaf size mesophyll 2, 6200-10000 mm**2; Leaf size mesophyll 3, 〉 10000 mm**2; Leaf size microphyll 1, 80-400 mm**2; Leaf size microphyll 2, 400-1400 mm**2; Leaf size microphyll 3, 1400-3600 mm**2; Leaf size nanophyll, 〈 5 mm**2; Lincang; NECLIME; NECLIME_campaign; Neogene Climate Evolution in Eurasia; ORDINAL NUMBER; Paleontological sampling; PALSAMP; Species; Yunnan, China
    Type: Dataset
    Format: text/tab-separated-values, 2016 data points
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