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三磷酸腺苷通过北部入口沼泽系统的流量。

Adenosine 5'-triphosphate flux through the north inlet marsh system.

机构信息

Belle W. Baruch Institute for Marine Biology and Coastal Research and Department of Biology, University of South Carolina, Columbia, South Carolina 29208.

出版信息

Appl Environ Microbiol. 1979 May;37(5):841-8. doi: 10.1128/aem.37.5.841-848.1979.

Abstract

The distribution, fluctuation, and short-term transport of total microbial biomass (measured as adenosine 5'-triphosphate [ATP]) was investigated in a large salt marsh creek. Hourly samples were collected synoptically for 25 h from 10 boats positioned across the 320-m width of the creek. Samples were collected from three depths ranging from 0.2 to 8.0 m. Hourly data obtained from each station were graphed, plotting depth against ATP. Subsequently, interpolated ATP values were generated for every one-tenth depth from the surface to the bottom with the use of an 11-point proportional divider. A total of 2,750 values were generated, and a mean value of 0.865 mg of ATP per m was determined. Maximum levels of ATP were found at high tide and minimal values were found at low tide. The distribution of ATP concentrations was found to be complex, with no suggestion of vertical stratification; however, horizontal divisions were apparent. ATP values corrected for direction of flow or velocity indicated two ebb-directed channels; however, when considered in total, there was a net import of ATP through the interface. The total import of ATP for this 25-h sampling period was calculated to be 3.58 kg, corresponding to a net transport of 39.8 mg of ATP per s through the cross section. Results suggest that detailed characterization of a creek transect in terms of ATP or any similar parameter requires the simultaneous measurements of both the concentration of the parameter in question and the velocity at the time and point from which the sample was taken.

摘要

总微生物生物量(以腺苷 5'-三磷酸 [ATP] 表示)的分布、波动和短期输运在一个大型盐沼溪中进行了调查。从 320 米宽的小溪的 10 艘船上同步收集了 25 小时的每小时样本。样本采集深度从 0.2 到 8.0 米不等。从每个站点获得的每小时数据都绘制了图表,将深度与 ATP 进行对比。随后,使用 11 点比例分配器从表面到底部为每十分之一的深度生成插值 ATP 值。共生成了 2750 个值,确定了 0.865 毫克/米的平均 ATP 值。ATP 的最高水平出现在高潮时,最低水平出现在低潮时。ATP 浓度的分布被发现很复杂,没有垂直分层的迹象;然而,水平分区是明显的。针对流向或速度校正的 ATP 值表明有两个退潮流向的通道;然而,当综合考虑时,通过界面有一个 ATP 的净输入。这个 25 小时采样期间的 ATP 总输入计算为 3.58 千克,相当于通过横截面对应的每秒 39.8 毫克的 ATP 净传输。结果表明,要详细描述 ATP 或任何类似参数的小溪横断面,需要同时测量该参数的浓度和采样时的速度。

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引用本文的文献

1
Transport of microbial biomass through the North Inlet ecosystem.
Microb Ecol. 1982 Oct;8(2):139-56. doi: 10.1007/BF02010447.
2
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3
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Microbiol Rev. 1980 Dec;44(4):739-96. doi: 10.1128/mr.44.4.739-796.1980.

本文引用的文献

1
The transport of microbial biomass and suspended material in a high-marsh creek.
Can J Microbiol. 1978 Jul;24(7):839-6. doi: 10.1139/m78-140.

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