Sandy shore benthic N2-fixation in Lake Malawi, Africa

M. Gondwe, S. Guildford, R. Hecky
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引用次数: 1

Abstract

Epipelic N2-fixation in Lake Malawi (9°30"S to l4°25"S) has been shown to be a very important local source of nitrogen (N) for epipelic algal growth, which supports highly diverse and populated endemic cichlid species (HIGGINS et al. 200 l). The rocky habitat, however, covers only about 30% of the lake's littoral area, while the remainder is almost entirely covered by sand (R.IBBINK et al. 1983). Despite sand covering a larger expanse of the littoral benthic zone with an almost entirely different biota from that of the rocky zone, N2-fixation in the lake's sand community has never been studied before. This is important particularly because algal growth in the lake has generally been perceived as N limited, which may become critical with the continued threat of eutrophication by increasing human populations and the associated land-use changes in the lake's catchment area (GUILDFORD et al. 2003). HECKY et al. (2003) showed that phosphorus (P) loading to the lake is increasing more rapidly than N loading, so that the epilimnion may become more N limited, thereby causing harmful N2-fixing cyanobacterial species to proliferate in the lake. We report results of a study conducted on 2 sandy beaches in the more productive southern part of Lake Malawi. Study objectives were to (l) estimate Nz-fixation rates on sandy sediments by using the acetylene reduction technique, and (2) evaluate the N input from epipsammic N2-fixation to the lake's epilimnion.
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非洲马拉维湖砂岸边底栖生物对n2的固定作用
马拉维湖(9°30”S至14°25”S)的上层浮游氮固定已被证明是上层浮游藻类生长的一个非常重要的本地氮(N)来源,它支持高度多样化和密集的地方性鲷鱼物种(HIGGINS等,2001)。然而,岩石栖息地仅覆盖了约30%的湖泊沿岸面积,而其余部分几乎完全被沙子覆盖(R.IBBINK等,1983)。尽管沙子覆盖了更广阔的沿海底栖区,其生物群与岩石区几乎完全不同,但湖泊沙子群落对n2的固定作用从未被研究过。这一点尤其重要,因为人们普遍认为湖泊中的藻类生长受到氮的限制,这可能对人口增加和湖泊集水区相关土地利用变化带来的持续富营养化威胁至关重要(GUILDFORD et al. 2003)。HECKY等(2003)研究表明,湖泊中磷(P)负荷的增加速度快于氮负荷的增加,从而使水体中的氮含量变得更加有限,从而导致有害的固氮蓝藻物种在湖泊中大量繁殖。我们报告了在马拉维湖南部高产的2个沙滩上进行的一项研究的结果。研究目的是:(1)利用乙炔还原技术估计沙质沉积物的氮固定率;(2)评估表层氮固定对湖泊表层氮的输入。
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