钒在海鞘和海藻中的作用

D. Rehder
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引用次数: 1

摘要

钒是海水中第二丰富的过渡金属,仅次于钼。含氧海水通常含有24-45 μM的钒酸H 2 VO 4(因此是仅次于钼的海水中第二丰富的过渡金属),其含量主要随季节而波动。约60%的损耗发生在VO的还原过程中,VO(OH) 2形成一种难溶的氢氧化物,极易被颗粒有机物吸收[1]。因此,影响钒发生的因素是氧化还原条件(如溶解的o2和Fe, nh3和S的存在,当然还有海洋生物对其的吸收。钒酸盐主要被海藻吸收,其中最突出的是结藻(又称岩草)Ascophyllum nodosum(图1),被海鞘吸收,在一定程度上也被一些多毛纲扇虫吸收[2]。钒作为这些生物的基本元素的重要性将被讨论。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
A Role for Vanadium in Ascidians and in Marine Algae
Vanadium is – next to molybdenum – the second-to-most abundant transition metal in sea water. Oxygenated sea water commonly contains 24-45 μM of vanadate H 2 VO 4 ˉ (and is thus – next to molybdenum – the second-to-most abundant transition metal in sea water) with the levels mainly fluctuating with the season. Depletion by about 60% can occur as reduction to VO takes place which forms a sparingly soluble hydroxide, VO(OH) 2 , that is readily absorbed by particulate organic matter [1]. Consequently, the factors influencing the occurrence of vanadium are redox conditions (such as dissolved O 2 and Fe, the presence of NH 3 and S , and – of course – its uptake by marine organisms. Vanadate is mainly taken up by marine algae, the most prominent one being knotted wrack (also known as rockweed) Ascophyllum nodosum, (Figure 1), by ascidians and, to some extent, also by some Polychaeta fan worms [2]. The significance of vanadium as an essential element in these organisms will be addressed.
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