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54篇 您的检索式:作者名="Munnecke"
    题名 作者 年代 出处 被引量
1Biostratigraphic and Chemostratigraphic Correlation for the Base of the Middle Ordovician between Yichang and Western Zhejiang Areas,South China显示文摘中间的奥陶纪的底(即 Dapingian 舞台) 在 conodont Baltoniodus 的第一本外观资料(一度时髦的风尚) 被定义 ? 在 Huanghuachang, Yichang,中国,而是到要决定的另外的外形遗体的区域的边界的精确关联的 triangularis。此处,我们考察 Huanghuachang 全球标准 Stratotype 节和点(GSSP ) 节的 biostratigraphy 和 chemostratigraphy,并且在 Yichang,和 Hengtang 石场节在附近的 Chenjiahe 节上介绍我们的最近的 stratigraphic 工作, Jiangshan,浙江,它斜坡外形被认为是代表性。象 Chenjiahe 节的 chemostratigraphy 一样的 conodont 和 graptolite biostratigraphy 显示中间的奥陶纪的库也在 graptolite Azygograptus suecicus 地区以内掉落,并且在一次次要的积极的碳同位素旅行以内与高或最大的 13C 值与一致,建议基础边界能乐意地越过全部 Yangtze 峡区域被认出。综合 graptolite 和 conodont biostratigraphy 和 Hengtang 节的 chemostratigraphy, Jiangshan,显示基础边界可能在 graptolite Isograptus caduceus imitatus 以内掉落躺 Azygograptus suecicus 地区,并且与 13C 的显著落下与一致的地区。这差别显示一条多学科的途径是批评的在在哪儿的那些区域识别基础边界 Baltoniodus ? triangularisZHANG Yuandong Axel MUNNECKE CHEN Xu CHENG Junfeng LIU Xiao 2011Acta Geologica Sinica(English Edition)2011,85,2:4
2Preliminary Estimation of Paleoproductivity via TOC and Habitat Types:Which Method Is More Reliable?—A Case Study on the Ordovician-Silurian Transitional Black Shales of the Upper Yangtze Platform, South China显示文摘New total organic carbon (TOC) data from the two Ordovician-Silurian transitional graptolite-bearing black shale intervals, the Wufeng (五峰) Formation and the Longmaxi (龙马溪) Formation in Central Guizhou (贵州) and West Hubei (湖北), respectively, as well as previously reported TOC data from the same intervals in other places on the Yangtze platform of South China, have been used to produce an initial estimate of the primary paleoproductivity via a conventional inverse method (i.e., Rpp-inverse). The values of the Rpp-inverse are estimated to be 32 (43-21) gC/(m2·a) (Wufeng Formation) and 21 (27-16) gC/(m2·a) (Longmaxi Formation). Also, simultaneously, the habitat types (i.e., HT; cf., BA: benthic assemblage) and their temporal and spatial changes have been documented from the same succession, and an initial estimate of the primary paleoproductivity has been produced using a forward method (i.e., Rpp-forward). Being bounded mainly by the peritidal to inner-shelf environment shelly-facies or mixed-facies successions with BA1 to BA3 faunas both at the top and the base, which indicates the habitat types from HT II1 to HT III2, the biohabitat type of the two graptolite-bearing black shale intervals can be limited to HT III to HT IV, corresponding to the inner shelf to the outer shelf, with depths from roughly 60 m to 200-300 m. Based on the current data from the South China Sea and the southern part of the East China Sea, values of Rpp-forward should be about 100 to 400 gC/(m2·a). The difference in the results via the two methods suggests that paleoproductivity estimates from the geological strata need to be made cautiously, with particular attention paid to the paleogeographic setting, oxic-anoxic conditions, as also the preservation factor of organic carbon.苏文博 王永标 Bradley D Cramer Axel Munnecke 李志明 傅力浦 2008Journal of China University of Geosciences2008,19,5:2
3Microbial decontamination of parathion and p -nitrophenol in aqueous media 显示文摘Munnecke D M Hsieh P D 1974Applied Microbio1974,28,2:1
4Enzymatic Detoxification of waste organophosphate pesticide显示文摘 1980Agric Food chem1980,28,1:1
5Microbial transformation of pesticide 显示文摘 1974Adv Appl Microbiol1974,18,:1
6Enzymatic detoxificaton of waste organophosphate pesticides 显示文摘Munnecke D M 1980Journal of Agricultural and Food Chemistry1980,28,:1
7Enzymatic detoxification of waste organophosphate pesticides显示文摘Munnecke D M 0,,:1
8Microbial decontamination of parathion and p-nitrophenol in aqueous media显示文摘Munnecke D M Dennis P H 1974Applied Microbiology1974,28,:1
9Ordovician and Silurian sea-water chemistry, sea level, and climate: A synopsis显示文摘Munnecke A Calner M David A T 2010Palaeogeography Palaeoclimatology Palaeoecology2010,296,:1
10Pathways of microbial metabolism of parathion显示文摘Munnecke D M Hsieeh D P 1976Appl Environ Microbiol1976,31,:1
11Ordovician and Silurian sea-water chemistry, sea level, and climate:a synopsis显示文摘Munnecke A Calner M Harper D A T 2010Palaeogeography Palaeoclimatology Palaeoecology2010,296,3:1
12Chemical, physical and biological methods for the disposal and detocifcation of pesticides 显示文摘 1979Residue Rev1979,70,:1
13Ordovician and Silurian sea–water chemistry, sea level, and climate: A synopsis显示文摘Axel Munnecke Mikael Calner David A.T. Harper Thomas Servais 2010Palaeogeography Palaeoclimatology Palaeoecology2010,,3:1
14Marine Sepiolite in Middle Permian Carbonates of South China: Implications for Secular Variation of Phanerozoic Seawater Chemistry 显示文摘Yah J X Munnecke A Steuber T 2005Journal of Sedimentary Research2005,75,3:1
15Microbial decontamination of parathion and p - nitrophenol in aqueous media 显示文摘Munnecke D M Hsieh D P H 1974Applied Microbiology1974,28,2:1
16Properties of an immobilized pesticide - hydrolyzing enzyme显示文摘Munnecke D M 1977Appl Environ Microbiol1977,33,3:1
17Microbial decontamination of parathion and p-nitrophenol in aqueous media显示文摘Munnecke D M Dennis P H 1974Applied Microbiology1974,28,:1
18Hydrolysis of organophosphate pesticides by an immobilized enzyme system显示文摘Munnecke D M 1979Biotechnol Bioeng1979,,22:1
19Hydrolysis of organophosphate pesticides by an immobilized enzyme system显示文摘Munnecke D M 1979Biotechnology and Bioengineering1979,22,:1
20Enzymic analysis of organophosphate insecticides using an enzyme thermistor显示文摘MATTIASSON B RIEKE E MUNNECKE G 1979Journal of Solid-Phase Biochemistry1979,4,4:1
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