水生苔藓植物中元素浓度的年循环变化

E. Núñez-Olivera, M. García-Álvaro, N. Beaucourt, J. Martínez-Abaigar
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引用次数: 15

摘要

在一年的周期内,每隔两周测定4种水下苔藓植物的7种元素(N、P、K、Ca、Mg、Fe和Na)的浓度:两种苔藓(解热藓和鳞藓),一种毛叶苔(Jungermannia exsertifolia subsp.)。桔梗草)和一种桔梗草(桔梗草)。正在考虑的假设是,它们的元素组成在一年中是否显示出季节性模式,如果是,这些变化是否取决于内部或环境因素。N、P、Na和Fe元素在年循环中出现频率最高,春季浓度最低,秋季浓度最高。我们的数据表明,季节周期取决于内部因素和环境因素的相互作用:1)水生苔藓植物营养生长的年循环,这导致植物组织内元素的稀释/浓度循环;2)部分树种(如荆芥)的年硬化特性变化;3)源流的物理和化学特征的时间变化。然而,在苔藓植物中某一特定元素的浓度与周围水体中该元素的浓度之间只发现了分散的相关性。因此,当考虑到苔藓植物元素组成的时间变化时,苔藓植物的行为不仅仅是元素的吸收者,而是更复杂的系统。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
Changes in element concentrations in aquatic bryophytes over an annual cycle
The concentrations of seven elements (N, P, K, Ca, Mg, Fe and Na) were measured every two weeks during an annual cycle, in four species of submerged aquatic bryophytes: two mosses (Fontinalis antipyretica and F. squamosa), a foliose liverwort (Jungermannia exsertifolia subsp. cordifolia) and a thalloid liverwort (Pellia endiviifolia). The hypothesis under consideration was whether their elemental composition over the year showed a seasonal pattern and, if so, whether those changes depended on internal or environmental factors. The elements showing most frequently an annual cycle were N, P, Na and Fe, and the most common temporal trend was that with the lowest concentrations appearing in spring and the highest ones in autumn. Our data suggest that the seasonal cycles depended on the interaction of both internal and environmental factors: 1) the annual cycle of vegetative growth in aquatic bryophytes, which causes a concomitant cycle of dilution/concentration of elements within the plant tissues; 2) the annual changes in sclerophylly in some species, such as J. cordifolia; and 3) the temporal variation in the physical and chemical features of the stream of origin. However, only scattered correlations were found between the concentrations of a given element in the bryophytes and the concentration of that element in the surrounding water. Thus, bryophytes do not behave as mere absorbers of elements, but more complex systems, when the temporal variation in their element composition is considered.
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