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Titlebook: Management von Familienunternehmen; Besonderheiten – Han Birgit Felden,Andreas Hack Textbook 20141st edition Springer Fachmedien Wiesbaden

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樓主: 鳴叫大步走
31#
發(fā)表于 2025-3-26 22:47:01 | 只看該作者
Birgit Felden,Andreas Hackquate karyotypic information (partly as a result of too few workers chasing too many organisms), and (3) the failure of their chromosomes to band satisfactorily. Compared to mammalian cytogenetics, our knowledge of marine invertebrates lags behind by several decades. With the current concern about m
32#
發(fā)表于 2025-3-27 01:22:52 | 只看該作者
33#
發(fā)表于 2025-3-27 06:09:24 | 只看該作者
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發(fā)表于 2025-3-27 12:16:22 | 只看該作者
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發(fā)表于 2025-3-27 16:18:29 | 只看該作者
36#
發(fā)表于 2025-3-27 21:47:39 | 只看該作者
37#
發(fā)表于 2025-3-27 22:13:59 | 只看該作者
Birgit Felden,Andreas Hackogeochemical cycles of marine sediments. Oxic respiration is by far the most important pathway of organic carbon in deep-sea sediments and significantly determines the recycling of organic matter introduced onto the sediment surface. Even if some uncertainty remains, benthic oxygen fluxes reveal pro
38#
發(fā)表于 2025-3-28 03:37:09 | 只看該作者
ogeochemical cycles of marine sediments. Oxic respiration is by far the most important pathway of organic carbon in deep-sea sediments and significantly determines the recycling of organic matter introduced onto the sediment surface. Even if some uncertainty remains, benthic oxygen fluxes reveal pro
39#
發(fā)表于 2025-3-28 07:10:09 | 只看該作者
Birgit Felden,Andreas Hackogeochemical cycles of marine sediments. Oxic respiration is by far the most important pathway of organic carbon in deep-sea sediments and significantly determines the recycling of organic matter introduced onto the sediment surface. Even if some uncertainty remains, benthic oxygen fluxes reveal pro
40#
發(fā)表于 2025-3-28 10:26:29 | 只看該作者
Birgit Felden,Andreas Hackogeochemical cycles of marine sediments. Oxic respiration is by far the most important pathway of organic carbon in deep-sea sediments and significantly determines the recycling of organic matter introduced onto the sediment surface. Even if some uncertainty remains, benthic oxygen fluxes reveal pro
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