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Earth's Phosphides in Levant and insights into the source of Archean prebiotic phosphorus

机译:黎凡特的地球上的磷化物以及对太古代益生元磷的来源的见解

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Natural phosphides - the minerals containing phosphorus in a redox state lower than zero – are common constituents of meteorites but virtually unknown on the Earth. Herein we present the first rich occurrence of iron-nickel phosphides of terrestrial origin. Phosphide-bearing rocks are exposed in three localities in the surroundings of the Dead Sea, Levant: in the northern Negev Desert, Israel and Transjordan Plateau, south of Amman, Jordan. Seven minerals from the ternary Fe-Ni-P system have been identified with five of them, NiP2, Ni5P4, Ni2P, FeP and FeP2, previously unknown in nature. The results of the present study could provide a new insight on the terrestrial origin of natural phosphides – the most likely source of reactive prebiotic phosphorus at the times of the early Earth.
机译:天然磷化物(一种氧化还原态的磷含量低于零的矿物)是陨石的常见成分,但实际上在地球上是未知的。在这里,我们提出了陆生来源的铁-镍磷化物的第一次丰富发生。黎凡特死海周围的三个地方都暴露有含磷的岩石:以色列北部的内盖夫沙漠和约旦安曼以南的Transjordan高原。从三元Fe-Ni-P系统中鉴定出7种矿物,其中5种为NiP 2 ,Ni 5 P 4 ,Ni < sub> 2 P,FeP和FeP 2 ,以前是未知的。本研究的结果可以为天然磷的地球起源提供新的见解-天然磷是地球早期的最有可能的活性益生元磷的来源。

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