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  • Spanish  (7)
  • Chinese  (1)
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  • 1
    Call number: AWI Bio-17-90819
    Description / Table of Contents: The authors completed collecting and arranging plates of photomicrographs for common pollen and spores in Quaternary strata. Given China's vast territory, complex vegetation types, a variety of plants, and polen grains with similar morphology probably produced by different plant species in different regions. We have organized this book's photomicrographs of pollen grains and spores in the division of China into five regions, i.e. northwest,northern, southeast, south and southwest China. Photomicrographs of pollen grains and spores in each region are arranged by plant classification system i.e. in order of algae, bryophyte, pteridophyte, gymnosperm, and angiosperm. All 409 plates of color photomicrographs for pollen grains and spores are finally illustrated and described.
    Description / Table of Contents: 本书整理编排了我国第四纪地层常见的孢粉类型显微照相图版,按照西北、北方、东南、华南和西南五个大区编排,并对这些区域的现代植被、第四纪植被史做了简要概述,还重点叙述了各地区第四纪主要孢粉类型、特点以及常见孢粉种类的鉴定形态特征。共分三章,第一章为我国各地区现代植被和第四纪植被概述,重点叙述了古植被与古气候的演变历史;第二章介绍本图鉴中所列出的各地区主要第四纪孢粉类型及其特点,并对不同地区常见孢粉种类
    Type of Medium: Monograph available for loan
    Pages: 620 Seiten , zahlreiche Illustrationen
    ISBN: 9787030505682
    Language: Chinese , Latin
    Note: Contents: Preface. - Chapter 1: Overview of modern and Quaternary vegetation in China. - 1.1 Northwest region / Tang Lingyu and Shen Caiming. - 1.1.1 Overview of modern vegetation. - 1.1.1.1 Gobi desert and desert vegetation in eastern Xinjiang. - 1.1.1.2 Extremely arid desert and shrubland vegetation in the Qaidam Basin. - 1.1.1.3 Arid desert shrub and semi-shrub vegetation in the Hexi Corridor. - 1.1.1.4 Sylvosteppe or pine-oak forest in the transitional region between semi-humid and semi-arid monsoonal climate of temperate zone in the Loess Plateau. - 1.1.2 Overview of Quaternary vegetation. - 1.1.2.1 Vegetation and environment since the early Pleistocene in Qinghai. - 1.1.2.2 Holocene vegetation succession of steppe/meadow in north Xizang (Tibet). - 1.1.2.3 Vegetation and environment since the late Pleistocene in the Loess Plateau. - 1.1.2.4 Vegetation and environment since the early Pleistocene in Xinjiang. - 1.2 Northern region / Tang Lingyu and Li Chunhai. - 1.2.1 Overview of modern vegetation. - 1.2.1.1 Coniferous and broadleaved forest and meadow of temperate zone in Northeast China. - 1.2.1.2 Oak forest of river valley, Chinese pine forest, and shrub steppe in the lower valley of Liaohe River, North China plain, southern Shanxi, and central Shaanxi plain. - 1.2.2 Overview of Quaternary vegetation. - 1.2.2.1 Vegetation and environment since the early Pleistocene in North China. - 1.2.2.2 Vegetation and environment since the early Pleistocene in Northeast China. - 1.3 Southeast region / Shu Junwu and Tang Lingyu. - 1.3.1 Overview of modern vegetation. - 1.3.2 Overview of Quaternary vegetation. - 1.3.2.1 Vegetation succession since the mid-Pleistocene in Hubei. - 1.3.2.2 Vegetation and environment since the late Pleistocene in the lower valley of the Yangtze River. - 1.3 .2.3 Forest succession since the last glaciation in southeast coast of Fujian. - 1.3.2.4 Vegetation and environment since the late Pleistocene in the central Taiwan. - 1.4 South region / Mao Limi, Tang Lingyu and Shen Cairning. - 1.4.1 Overview of modern vegetation. - 1.4.1.1 Vegetation in the southern zone of middle subtropical evergreen broadleaved forest. - 1.4.1.2 Vegetation in the zone of south subtropical evergreen broadleaved forest. - 1.4.1.3 Tropical semi-evergreen monsoonal forest and tropical monsoonal forest. - 1.4.2 Overview of Quaternary vegetation. - 1.4.2.1 Vegetation in the Zhujiang delta and Chaozhou plain since the Pleistocene recorded by pollen and spores. - 1.4.2.2 Vegetation and climate since the late Pleistocene in Leizhou Peninsula and Holocene vegetation and climate in Hainan Island. - 1.4.2.3 Late Quaternary pollen and spores, vegetation and climate records in the South. - 1.4.2.4 Vegetation and climate since the late Pleistocene in Hong Kong. - 1.5 Southwest region / Shu Junwu, Tang Lingyu and Shen Caiming. - 1.5.1 Overview of modern vegetation. - 1.5.1.1 Vegetation of evergreen broadleaved forest in the Yunnan , Guizhou and western Sichuan Plateau. - 1.5.1.2 Vegetation of coniferous forest in southeast Xizang. - 1.5.2 Overview of Quaternary vegetation. - 1.5.2.1 Holocene vegetation in northwest Yunnan. - 1.5.2.2 Vegetation and monsoonal climate history since the late Pleistocene in western and south-central Yunnan. - 1.5.2.3 Holocene vegetation in western Sichuan. - 1.5.2.4 Vegetation and environment since the late Pleistocene in Guizhou. - 1.5.2.5 Vegetation and monsoonal climate history since the late Pleistocene in southeastern Xizang. - Chapter 2 Main types of Quaternary pollen and spores and their characteristics in different regions of China. - 2.1 Northwest region / Tang Lingyu and Mao Limi. - 2.1.1 Types of Quaternary pollen and spores in Northwest China. - 2.1.2 Identifiable features of major Quaternary pollen and spores in Northwest China. - 2.1.2.1 Identifiable features of main Compositae pollen types. - 2.1.2.2 Identifiable features of Artemisia, Tamarix, and Zygophyllum pollen. - 2.1.2.3 Identifiable features of Rhamnus, Hippophae, and Elaeagnus pollen. - 2.1.3 Descriptions of morphological features for major Quaternary spores and pollen in Northwest China. - 2.1.3.1 Photomicrographs for major Quaternary pollen types in Northwest China. - 2.1.3.2 Descriptions of morphological features for major Quaternary pollen types in Northwest China. - 2.2 Northern region / Tang Lingyu. - 2.2.1 Types of Quaternary pollen and spores in Northern China. - 2.2.2 Identifiable features of major Quaternary pollen and spores in Northern China. - 2.2.2.1 Identification keys of pollen morphology for several saccate genera of Pinaceae. - 2.2.2.2 Identifiable features of pollen morphology for genera of Betulaceae. - 2.2.2.3 Identifiable features of tricolpate pollen from Salix and Cruciferae. - 2.2.2.4 Identifiable features of tricolpate pollen from Ranunculaceae and Labiatae. - 2.2.3 Descriptions of morphological features for major Quaternary spores and pollen in Northern China. - 2.2.3.1 Photomicrographs for major Quaternary pollen types in Northern China. - 2.2.3.2 Descriptions of morphological features for major Quaternary pollen types in Northern China. - 2.3 Southeast region / Tang Lingyu and Shu Junwu. - 2.3.1 Types of Quaternary pollen and spores in Southeast China. - 2.3.2 Identifiable features of major Quaternary pollen and spores in Southeast China. - 2.3.2.1 Identifiable features of pollen morphology for Fagaceae. - 2.3.2.2 Identification keys of pollen morphology for several genera of Fagaceae. - 2.3.2.3 Identifiable features of pollen morphology for several genera of Fagaceae. - 2.3.2.4 Identifiable features of pollen morphology for several genera of tropical and subtropical. - 2.3.3 Descriptions of morphological features for major Quaternary pollen and spores in Southeast China. - 2.3.3.1 Photomicrographs for major Quaternary pollen types in Southeast China. - 2.3.3.2 Descriptions of morphological features for major Quaternary pollen types in Southeast China. - 2.4 South region / Mao Limi and Tang Lingyu. - 2.4.1 Types of Quaternary pollen and spores in South China. - 2.4.2 Identifiable features of main Quaternary pollen and spores in South China. - 2.4.2.1 Modern distribution and paleophytogeography of Sonneratia and its identifiable features of pollen morphology. - 2.4.2.2 Modern distribution and paleoecology significance of Rhizophoraceae and its identifiable features of pollen morphology. - 2.4.3 Photomicrographs and descriptions of morphological features for major Quaternary pollen and spores in South China. - 2.4.3.1 Photomicrographs for major Quaternary pollen and spores in South China. - 2.4.3.2 Descriptions of morphological features for major Quaternary pollen and spores in South China. - 2.5 Southwest region / Tang Lingyu and Shu Junwu. - 2.5.1 Types of Quaternary pollen and spores in Southwest China. - 2.5.2 Identifiable feature of main Quaternary pollen and spores in Southwest China. - 2.5.2.1 Plant distribution and pollen features of Pinaceae in Southwest China. - 2.5.2.2 Identification keys of pollen morphology for Pinaceae. - 2.5.3 Descriptions of morphological features for major Quaternary pollen and spores in Southwest China. - 2.5.3.1 Photomicrographs for common pollen in Southwest China. - 2.5.3.2 Descriptions of morphological features for major Quaternary pollen and spores in Southwest China. - Chapter 3 Plates and descriptions of Quaternary pollen and spores in different region of China. - 3.1 Northwest region / Tang Lingyu and Mao Limi. - Spores of the pteridophyte Plates 1-3. - Gymnosperm pollen Plates 3-10. - Angiosperm pollen Plates 11-63. - 3.2 Northern region / Tang Lingyu and Li Chunhai. - Spores of the algae Plates 1-3. - Spores of the bryophyte Plate 4. - Spores of the pteridophyte Plates 5-9. - Gymnosperm pollen Plates 9-24. - Angiosperm pollen Plates 25-63. - 3.3 Southeast region / Tang Lingyu, Zhou Zhongze and
    Location: AWI Reading room
    Branch Library: AWI Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Madrid : Secc
    Call number: PIK N 456-17-90913
    Type of Medium: Monograph available for loan
    Pages: 536 Seiten
    Series Statement: Ministerio de Transportes Turismo Y Comunicaciones : Publicación Serie A 114
    Parallel Title: 1,1=6; 2,1=13 von Publicaciones / D / Ministerio del Aire, Subsecretaria de Aviación Civil, Servicio Meteorológico Nacional
    Language: Spanish
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 3
    Publication Date: 2021-03-29
    Description: Dada la importancia que revisten los suelos en los procesos que ocurren en la zona crítica (zona de interacción entre agua, suelo, aire, organismos), en este trabajo presentamos la distribución temporal y espacial de una secuencia de paleosuelos arcillosos con carbonatos secundarios (capas de caliches y carbonatos diseminados) en el sector nororiental de la Cuenca de México, particularmente en el valle de Teotihuacán. El propósito de este trabajo consiste en reconstruir la distribución temporal y espacial de la cubierta de suelos del pasado para entender su relación con la estructura actual de suelos y sedimentos en este sector semiárido de la cuenca de México. Con esta información, determinar la participación de estos materiales en la Zona Crítica (ZC). Para ello, se ha llevado a cabo un transecto de dirección norte-sur, que inicia en las elevaciones del Cerro Gordo, cruza el valle de Teotihuacán y termina en la Sierra Patlachique, describiendo perfiles de suelo en diferentes posiciones geomorfológicas. El marco cronológico se ha establecido con base en fechamientos de radiocarbono realizados en las capas de caliches. De acuerdo a la cronología, al tipo y grado de pedogénesis, y a los procesos de sedimentación, se han reconocido cuatro unidades. La primera unidad, denominada Paleosuelos del Pleistoceno, fase I (50000 – 20000 años AP), está compuesta de paleosuelos arcillosos, los cuales son Luvisoles crómicos y estágnicos, dependiendo de su posición en el paisaje. Estos paleosuelos muestran tanto carbonatos secundarios diseminados y en fracturas, como capas de caliches. En la segunda unidad, Paleosuelos del Pleistoceno, fase II (20000 –10000 años AP), dominan los sedimentos sobre los suelos; únicamente en el fondo del Valle, se han encontrado Gleysoles cortados por canales aluviales. La unidad, Paleosuelos del Holoceno, fase I (10000 a 1000 años AP) se caracteriza por presentar suelos poligenéticos (Vertisoles), fuertemente modificados por los procesos antrópicos, durante las diversas fases de ocupación pre-hispánica. La última unidad, Suelos del Holoceno, fase II, abarca el último milenio, en donde se destacan procesos de erosión e inestabilidad del paisaje. La tendencia principal en la distribución espacial de los paleosuelos es la siguiente: las unidades antiguas (Luvisoles, capas de caliches y Vertisoles) están sepultadas profundamente en el fondo del valle. Sin embargo, en los taludes y elevaciones montañosas, pueden aparecer cerca o directamente sobre la superficie, siendo incorporados en el manto de suelos actual. Las interrelaciones entre los diferentes paleosuelos a lo largo del transecto estudiado, junto con las observaciones micromorfológicas, apoyan la hipótesis de una relación evolutiva entre los Luvisoles pleistocénicos y los Vertisoles del Holoceno. Consideramos que estas diferentes unidades repercuten en los procesos hidrológicos en el valle y que las capas de caliche formadas en los ambientes pleistocénicos pueden afectar la geoquímica del agua subterránea así como sus firmas isotópicas.
    Description: As soils are important elements for the processes involved in the critical zone (the zone of interaction between water, soil, air, and organisms), in this work we present the temporal and spatial distribution of a clayey-paleosol sequence with secondary carbonates (layers of caliche and disseminated carbonates) in the northeast sector of the Mexico Basin, particularly in the Teotihuacan Valley. The goal of this paper is the temporal and spatial reconstruction of the past soil cover to understand its relationship with the present day soils and sediments in this semiarid sector of the Mexico Basin. With this information the involvement of these materials in the critical zone could be determined. To comply with these objectives, a north-south transect was carried out, starting in the Cerro Gordo, crossing the Teotihuacan valley and ending in the Sierra Patlachique, describing soil profiles located in different geomorphological positions. The chronological framework has been established with radiocarbon dates of the caliche layers. According to this chronology, the type and degree of pedogenesis, as well as the sedimentation processes, four units have been recognized. The first unit is named the Pleistocene Paleosols, phase I (50000 – 20000 years BP), and is composed of clayey paleosols, chromic and stagnic Luvisols, depending on their position in the landscape. These paleosols contain pedogenic carbonates, disseminated and in fractures, and caliche layers. In the second unit, the Pleistocene Paleosols, phase II (20000 –10000 years BP), sediments predominate over soils; only in the valley floor some Gleysols are found to be cut by alluvial channels. The unit, Paleosols of the Holocene Paleosols unit, phase I (10000 to 1000 years BP), is characterized by polygenetic soils (Vertisols) strongly modified by anthropic processes during distinct phases of pre-hispanic occupation. The last unit, the Holocene Soils, phase II, covers the last millennium when erosional processes and unstable landscape dominate. The paleosols (Luvisols, caliche layers, and Vertisols) are deeply buried at the bottom of the valley. However, on the slopes and hilltop positions, they can appear close to or directly on the surface, being incorporated in the present day soil mantle. Spatial interrelations of different paleosols along the studied transect together with micromorphological observations support the hypothesis of an evolutionary link between the Pleistocene Luvisols and the Holocene Vertisols. We propose that these different units are involved in the hydrological processes in the valley and that the caliche layers, formed in the Pleistocene environments, can affect the geochemistry of the groundwater as well as its isotopic signatures.
    Keywords: paleosuelos; Teotihuacán; caliches; Luvisoles; Vertisoles; cuenca de México; paleosols; Teotihuacan; caliches; Luvisols; Vertisols; Basin of Mexico ; 551
    Language: Spanish
    Type: article , publishedVersion
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  • 4
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    Ciudad de México : Fundación Friedrich Ebert en México
    Publication Date: 2019-01-18
    Keywords: ddc:320
    Repository Name: Wuppertal Institut für Klima, Umwelt, Energie
    Language: Spanish
    Type: report , doc-type:report
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  • 5
    Publication Date: 2020-02-12
    Description: Las fechas claves para la reunión científica del grupo de Paleomagnetismo de Iberia, MAGIBER X. (14, 15 y 16 de Septiembre de 2017, Valle del Grío, Provincia de Zaragoza) Desde sus inicios en el año 2001, el grupo de Paleomagnetismo de Iberia ha realizado reuniones de carácter periódico, generalmente bianuales. Estas reuniones se han caracterizado por su carácter familiar y cercano, en busca de la interacción positiva entre las personas que aúnan en sus estudios las ciencias de la tierra y el magnetismo, en todas sus disciplinas. Por ello, son bienvenidos trabajos de investigación en todas sus fases de desarrollo, ya sean trabajos finalizados o trabajos en estado de desarrollo que permitan la discusión entre los asistentes, e incluso puedan ayudar con sus sugerencias a la finalización de los mismos. También son recibidos otros trabajos que, si bien no totalmente relacionados, puedan permitir nuevas líneas de colaboración con otras disciplinas, pues si algo caracteriza al paleomagnetismo s.l. es su gran aplicabilidad en numerosos campos, diferentes entre sí.
    Language: Spanish
    Type: info:eu-repo/semantics/conferenceObject
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  • 6
    Publication Date: 2023-07-18
    Description: Motivated by the question of how the arts can contribute to communication on sustainable development, this study makes a sociological-anthropological analysis of the reception of an international contemporary art exhibition on sustainability in Valparaíso, Chile. The public’s aesthetic experience demonstrates that art, through sensual components and aesthetic strategies that lead to reflection can advance susceptibility to questions of sustainable development. This potential can point to gaps in the local public discussion on sustainability, but it is not capable of filling them.
    Language: Spanish
    Type: info:eu-repo/semantics/article
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  • 7
    Publication Date: 2023-07-18
    Description: Este informe demuestra que existe tanto la necesidad como la oportunidad de aumentar la interacción entre los niveles regional y mundial de la gobernanza de los océanos mediante un nuevo acuerdo mundial para la conservación y el uso sostenible de la diversidad biológica marina en las áreas fuera de la jurisdicción nacional (ABNJ, por sus siglas en inglés). En particular, este informe de política tiene por objeto destacar el papel y la contribución de la gobernanza regional y sectorial en elaborar y apuntalar la aplicación de un acuerdo fuerte en alta mar. Los esfuerzos regionales ofrecen lecciones aprendidas, plataformas para el intercambio de datos y conocimientos científicos, mecanismos para convocar a los Estados y las partes interesadas y coordinar los enfoques y medidas regionales para la gestión. Este informe identifica las oportunidades para aumentar la coordinación, la cooperación y la acción entre estos dos niveles en vista de un acuerdo internacional jurídicamente vinculante eficaz en el marco de la Convención de las Naciones Unidas sobre el Derecho del Mar (CONVEMAR).
    Language: Spanish
    Type: info:eu-repo/semantics/workingPaper
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  • 8
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    In:  Desacatos Revista de Antropología Social
    Publication Date: 2023-07-18
    Language: Spanish
    Type: info:eu-repo/semantics/article
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