Capone D G, Taylor B F
Can J Microbiol. 1980 Aug;26(8):998-1005. doi: 10.1139/m80-169.
N2 fixation (C2H2 reduction) associated with the roots, rhizomes, and sediments (rhizosphere cores) of the seagrass Thalassia testudinum was measured at sites in South Florida (Soldier Key, Biscayne Bay) and the Bahamas (Bimini Harbor). Rates of C2H2 reduction were higher in anaerobic than in aerobic assays and were linear for several hours after an initial lag period of 1-2h. Nitrogenase activity was proportional to the weight of rhizomes plus roots but showed no correlation with the total weight of the rhizosphere cores. C2H2 reduction occurred to depths of at least 30 cm but the majority (<85%) of the activity was in the 0- to 20-cm fraction; also the ratio of activities for the 0- to 10- and 10- to 20-cm depths was about 2:1. Most investigations were carried out using anaerobic assays of the 0- to 10-cm fractions and rates calculated for the period of 3-6 h after adding C2H2. These rates were not stimulated by organic compounds (glucose, lactate, succinate) but were approximately halved by a decrease in temperature of 10 degrees C. In a seasonal study at Soldier Key the rates of N2 fixation varied about 20-fold with maximal rates in late summer and minimal rates in winter (January). On a diurnal basis, C2H2 reduction increased in the morning but was depressed in midafternoon, probably due to O2 buildup in the rhizosphere. Daily rates of N2 fixation, during the summer months of 1975-1978, varied between 5 and 24 mg N (-2)m and the estimated annual rates of N2 fixation were 10-50 kg N (-1)ha, taking into account seasonal variations and activities to a depth of 20 cm.
在南佛罗里达州(士兵礁、比斯坎湾)和巴哈马群岛(比米尼港)的一些地点,对与海草泰来草的根、根状茎及沉积物(根际土样)相关的N₂固定(C₂H₂还原)进行了测量。在厌氧测定中,C₂H₂还原速率高于需氧测定,并且在最初1 - 2小时的滞后期后,在数小时内呈线性关系。固氮酶活性与根状茎加根的重量成正比,但与根际土样的总重量无关。C₂H₂还原发生在至少30厘米的深度,但大部分(<85%)活性存在于0至20厘米的部分;而且0至10厘米和10至20厘米深度的活性比率约为2:1。大多数研究是使用0至10厘米部分的厌氧测定法进行的,并计算添加C₂H₂后3至6小时期间的速率。这些速率不受有机化合物(葡萄糖、乳酸盐、琥珀酸盐)的刺激,但温度降低10摄氏度时,速率大约减半。在士兵礁进行的一项季节性研究中,N₂固定速率变化约20倍,夏末时速率最高,冬季(1月)时速率最低。在昼夜基础上,C₂H₂还原在早晨增加,但在下午中段受到抑制,这可能是由于根际中氧气积累所致。在1975 - 1978年夏季月份,每日N₂固定速率在5至24毫克N(-2)m之间变化,考虑到季节性变化以及20厘米深度的活性,估计的年N₂固定速率为10 - 50千克N(-1)公顷。