Complex lessons of iron uptake

Richard J. Geider

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Complex lessons of iron uptake

机译：铁吸收的综合课程

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Oceanographers often speak of physical or chemical pressure on primary ocean productivity (that is, the pho-tosynthetic conversion of CO_2 to new organic matter), but there is increasing evidence that marine phytoplankton also influence the fertility of the sea through production and consumption of dissolved organic compounds. This is the case for copper, which is detoxified by the release of specific organic ligands into the sea by planktonic bacteria. It is also true for iron dissolved in the sea, of which 99% is bound to organic ligands in a way that actually increases the availability of this essential nutrient.

机译：海洋学家经常谈到对初级海洋生产力的物理或化学压力（即，CO_2的光合作用转化为新的有机物），但是越来越多的证据表明，海洋浮游植物还通过溶解性物质的生产和消费来影响海洋的肥力。有机化合物。铜就是这种情况，铜可以通过浮游细菌将特定的有机配体释放到海洋中来排毒。溶解在海中的铁也是如此，其中99％的铁与有机配体结合，从而实际上增加了这种必需营养素的利用率。

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《Nature》 |1999年第6747期|p.815-816|共2页
作者
Richard J. Geider;
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收录信息美国《科学引文索引》(SCI);美国《工程索引》(EI);美国《生物学医学文摘》(MEDLINE);美国《化学文摘》(CA);
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正文语种 eng
中图分类自然科学总论;
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Complex lessons of iron uptake

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