泥炭地特征性环境因子促进泥炭藓持久孢子库的形成
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冯璐,卜兆君,吴玉环,刘莎莎,刘超
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Characteristic environmental factors in peatlands facilitate the formation of persistent Sphagnum spore banks
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FENG Lu,BU Zhao-Jun,WU Yu-Huan,LIU Sha-Sha,LIU Chao
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表2 三种保存液的主要化学元素和总酚浓度(mg·L-1)(平均值±标准误差, n = 3)
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Table 2 Main chemical elements and total phenolics concentration (mg·L-1) in three solutions (mean ± SE, n = 3)
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| TN | TP | K+ | Ca2+ | Na+ | Mg2+ | 总酚 Phenolics | | 超纯水 Ultrapure water | 0.00 ± 0.00c | 0.00 ± 0.00c | 0.00 ± 0.00c | 0.05 ± 0.01c | 0.00 ± 0.00c | 0.02 ± 0.00c | 0.00 ± 0.00c | 泥炭地地表水 Peatland surface water | 0.52 ± 0.05b | 0.03 ± 0.01b | 2.90 ± 0.33b | 5.22 ± 0.70a | 1.64 ± 0.16b | 1.43 ± 0.12a | 6.51 ± 0.05a | 中位泥炭藓沥出液 Leachate water of Sphagnum magellanicum | 5.03 ± 0.31a | 0.26 ± 0.04a | 8.89 ± 1.13a | 0.71 ± 0.49b | 4.33 ± 0.18a | 0.39 ± 0.06b | 3.23 ± 0.09b |
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