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Microminerals

机译:微量矿物质

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摘要

A while ago, I was working away at the microscope when an insect suddenly appeared in my field of view. This happens to all of us from time to time. Usually, it's a tiny wanderer from field collecting, and though startling, it's not surprising. This one, however, was a surprise. It was dead, and it was not on the specimen, but in the specimen. As Figure 1 shows, it was under a layer of thermonatrite (Na_2CO_3 centre dot H_2O). Thermonatrite usually derives from the dehydration of natron (Na_2CO_3 centre dot 10H_2O), and there's plenty of natron in Mont Saint-Hilaire, where the specimen originated. The origin of the thermonatrite was clear. What was not clear (and still isn't) is why the insect was under the thermonatrite and not on top of it. Thermonatrite effloresces from cracks containing natron, but it shouldn't be climbing on top of things like bugs. A quick check with the Canadian Museum of Nature revealed that the insect was a silken fungus beetle (Cryptophagidae, probably caenoscelis), possibly from the forest floor above the quarry. As a bio-mineral specimen, it doesn't equate to malachite pseudomorphs after mice (like the one Rock Currier once reported having seen in the Fers-man Museum in Moscow), but at 2 mm from stem to stern, it's the right scale for micromounters!
机译:前一阵子,我正在显微镜下工作,当时昆虫突然出现在我的视野中。这不时发生在我们所有人身上。通常,这是来自野外采集的微小游荡者,尽管令人吃惊,但这并不奇怪。然而,这是一个惊喜。它已经死了,它不在标本上,而是在标本上​​。如图1所示,它位于热钠盐(Na_2CO_3中心点H_2O)的下面。菱铁矿通常来自于中子的脱水(Na_2CO_3中心点10H_2O),并且在标本起源的Mont Saint-Hilaire中有大量的中子。萤石的起源很清楚。尚不清楚(现在仍然不是)的是,为什么昆虫在热钠盐之下而不是在其顶部。 Thermonatrite的风起因于含有natron的裂缝,但不应爬在虫子之类的东西上。对加拿大自然博物馆的快速检查显示,该昆虫是一种丝状真菌甲虫(隐孢子虫,可能是caenoscelis),可能来自采石场上方的森林地面。作为一种生物矿物标本,它不等同于老鼠后的孔雀石假晶体(就像曾经报道过在莫斯科费斯曼博物馆见过的一只岩咖),但是从茎到尾只有2毫米,这是正确的尺度适用于微型安装器!

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