美国俄克拉何马州盐平原国家野生动物保护区藻类生物量与理化特性的原位研究。

Kelly M Major, Andrea E Kirkwood, Clinton S Major, John W McCreadie, William J Henley
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引用次数: 17

摘要

这是一系列实验中的第一个,旨在描述俄克拉荷马州西北部盐平原国家野生动物保护区(SPNWR)的生态系统,并对其微生物居民进行分类。SPNWR是古代海洋的遗迹,包括大约65平方公里的高盐平地,由阿肯色河的支流提供水源。2000年7月至2001年7月,采用巢式块设计对3个永久站点的相对藻类生物量(即叶绿素浓度)和理化参数进行了为期1年的监测。这些公寓的显著特征包括年气温在-10到40摄氏度之间,与其他干旱/半干旱环境相似,每天15-20度的波动很常见。公寓系统中没有阴影;强辐射和高温(空气和沉积物表面)导致整个西北水区的可用水量很低,沉积物表面的水平仅为15%左右。此外,每日的中等风速是恒定的(约8-12公里每小时),有时最高风速可达137公里每小时。典型的淡水系统中,正磷酸盐(PO(4)3-)的浓度很低,在0.04 ~ 0.03之间
本文章由计算机程序翻译,如有差异,请以英文原文为准。

In situ studies of algal biomass in relation to physicochemical characteristics of the Salt Plains National Wildlife Refuge, Oklahoma, USA.

In situ studies of algal biomass in relation to physicochemical characteristics of the Salt Plains National Wildlife Refuge, Oklahoma, USA.

In situ studies of algal biomass in relation to physicochemical characteristics of the Salt Plains National Wildlife Refuge, Oklahoma, USA.

In situ studies of algal biomass in relation to physicochemical characteristics of the Salt Plains National Wildlife Refuge, Oklahoma, USA.

This is the first in a series of experiments designed to characterize the Salt Plains National Wildlife Refuge (SPNWR) ecosystem in northwestern Oklahoma and to catalogue its microbial inhabitants. The SPNWR is the remnant of an ancient ocean, encompassing approximately 65 km2 of variably hypersaline flat land, fed by tributaries of the Arkansas River. Relative algal biomass (i.e., chlorophyll concentrations attributed to Chlorophyll-a-containing oxygenic phototrophs) and physical and chemical parameters were monitored at three permanent stations for a one-year period (July 2000 to July 2001) using a nested block design. Salient features of the flats include annual air temperatures that ranged from -10 to 40 degrees C, and similar to other arid/semi-arid environments, 15-20-degree daily swings were common. Shade is absent from the flats system; intense irradiance and high temperatures (air and sediment surface) resulted in low water availability across the SPNWR, with levels of only ca. 15 % at the sediment surface. Moreover, moderate daily winds were constant (ca. 8-12 km h-1), sometimes achieving maximum speeds of up to 137 km h-1. Typical of freshwater systems, orthophosphate (PO(4)3-) concentrations were low, ranging from 0.04 to <1 microM; dissolved inorganic nitrogen levels were high, but spatially variable, ranging from ca. 250-600 microM (NO(3)- + NO(2)-) and 4-166 microM (NH(4)+). Phototroph abundance was likely tied to nutrient availability, with high-nutrient sites exhibiting high Chl-a levels (ca. 1.46 mg m-2). Despite these harsh conditions, the phototrophic microbial community was unexpectedly diverse. Preliminary attempts to isolate and identify oxygenic phototrophs from SPNWR water and soil samples yielded 47 species from 20 taxa and 3 divisions. Our data indicate that highly variable, extreme environments might support phototrophic microbial communities characterized by higher species diversity than previously assumed.

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