『新东方在线托福听力』为托福考生准备了ETS托福TPO/Official 39 Lec 1听力练习：What similarities does the professor point out between minerals and living organisms?原文题目答案解析，TPO/Official 39 Lec 1听力原文范文音频翻译。

托福TPO/Official 39 Lec 1听力原文What similarities does the professor point out between minerals and living organisms?【新东方在线】

旁白：请听一段地质学讲座的节选片段。

Narrator: Listen to part of a lecture in a geology class.

教授：自从地球在45亿年前形成开始，地球上的矿物种类的数量就发生了急剧增长，从只有仅仅几种相对简单的矿物质增长到4300多种我们现在可以识别的矿物，其中的很多矿物很复杂。

Professor: Since Earth formed some four and a half billion years ago, the number of minerals here has increased dramatically, from a few dozen relatively simple minerals early on to over 4,300 kinds of minerals we can identify today, many of them wonderfully complex.

一个地质学的基本问题是，这些新的矿物质是怎么形成的。

A basic question of geology is how all these new minerals came into being.

近期的研究转向了生物学，以求解释这些新生矿物的产生过程。

Well, recent studies have turned to biology to try to explain how this happens.

生物学的大部分理论是通过进化的视角来研究的。

Now, much of biology is studied through the lens of evolution.

进化的理论意思是，随着环境的改变，当然环境不可避免地一直在改变，一些有机物会产生让它们成功适应环境的特征，这些特征帮助这些有机物生长存活下来，再产生后代。

And the theory of evolution suggests that as environments change, and inevitably they do, some organisms will have characteristics that allow them to adapt to those changes successfully, characteristics that help these organisms develop and survive, and reproduce.

当环境变得更加复杂的时候，这也是一直在发生的事情，这一些早期的生物的变异会成为特征结合和进一步变异的基础，进一步产生更加多样和复杂的生命。

And when environments become more complex, as tends to happen over time, those earlier adaptations, those variations, become the basis of yet other combinations and variations, and lead to ever more diverse and complex forms of life.

所以从十亿年前数量少的、简单的和相对来说更加相似的生命形式，地球上的生物现在变成了一群有巨大多样性和复杂性的群体。

So from fewer, simpler and relatively similar forms of life billions of years ago, life on Earth has now become a dazzling array of diversity and complexity.

一些地质学家现在想把这个理论应用到解释矿物质多样性上。

Well, some geologists now want to apply this concept to explain mineral diversity too.

矿物质所处的环境不是一成不变的，譬如温度、压强或者化学环境是一直在变化的。

The conditions that minerals are under are not constant, conditions like temperature, or pressure, or chemical surroundings.

这一些变化，经常是循环往复发生，随着时间增强或者减弱。

These change, often in cycles, increasing and decreasing slowly over time.

随着环境的改变，矿物质有时候会分解。

And as conditions change, minerals sometimes break down.

它们的原子重新组合成为新的化合物，这就是一个称为矿物质进化的过程的一部分。

And their atoms recombine into totally new compounds as part of a process some called mineral evolution.

矿物质肯定不是活物，所以矿物质进化的概念和生物进化的概念是不同的，但是还是有很多过程是平行的。

Now, minerals are not alive of course, so this is not evolution in quite the same sense you'd have in living organisms, but there do appear to be some parallels.

活体生物不仅仅要适应环境，还去改变环境，改变环境以后，这个环境可能会变得适宜其他有机体生长。

Living organisms not only adapt to their environment, but also affect it, change the environment within which other organisms may then develop.

类似地，每一种新的矿物质同样会丰富其化学环境，而这个化学环境是很多其他更复杂的矿物质未来会产生的发源地。

Likewise, each new mineral also enriches the chemical environment from which lots of other even more complex new minerals may be formed in the future.

除了这些相似点，矿物质进化的吸引人的一点是矿物质显然是和有机物一起进化的。

Beyond these similarities though, what's really fascinating about mineral evolution is the way minerals apparently coevolve with living organisms.

也许是十亿年以前，在地球形成之后，我们第一次发现了生命存在的证据。

Well, it's maybe a billion years after Earth's formation that we first see evidence of life.

当然了早期的生命体是很基础的，就仅仅是小小的、单细胞的生物，但是随着时间过去，它们起到了深远的作用。

Of course early life forms were primitive, just tiny, single-celled microbes, but overtime, they had a profound effect.

大量的这种微生物开始通过光合作用生产养料，光合作用释放了大量的氧气，氧气导致和当时存在的矿物质反应，形成了例如铁锈一样的东西，这些物质再和大范围的不同金属反应，最终产生多种矿物质。

Huge numbers of these microbes began producing food by photosynthesis, which of course also freed up enormous amounts of oxygen and lots of that oxygen interacted with the atoms of existing minerals, creating rust out of iron for instance, reacting with a whole range of different metals to create lots of new minerals.

微生物依赖矿物质而生存，但是它们并不是仅仅把矿物质作为营养物质而吸收，他们还分泌一些别的矿物质作为排泄物，包括我们称为生物矿物质的东西，这种物质是通过有机体的帮助下产生的。

Now, living organisms rely on minerals, but they not only take in some minerals as nutrients, they also excrete others as waste products, including what we call bio minerals, minerals that form with the help of biological life.

我们可以通过叠层石得到地质学上关于生物矿物质产生的证据。

We can see geologic evidence of bio mineral production in what are called stromatolites.

叠层石看起来像是一层层的沉积岩，但它们其实是化石，是微生物的一层层的残渣。

Stromatolites look like wavy layers of sedimentary rock, but they are really fossils, fossils of the waste from microbial mats.

微生物层时一大片单细胞生物，这些生物曾经是地球上最占优势的物种。

microbial mats are vast colonies of one-celled organisms that were once the most prevalent form of life on Earth.

针对叠层石的研究发现这些古代微生物层会与环境中的矿物质发生相互作用，产生新的化合物残渣。

And the study of stromatolites indicates that these ancient microbial mats interacted with minerals in the environment and left behind new compounds as waste products.

这种生物矿物质就是，例如碳酸盐、磷酸盐和二氧化硅这样的物质。

Bio minerals like carbonates, phosphates, and silica.

实际上，我们已经可以在实验室里培养微生物层。

In fact, we've grown microbial mats in the laboratory.

随着时间的过去，它们也开始产生我们在叠层石里发现的相同的矿物质。

And over time, they too have produced some of the same sorts of minerals found in stromatolites.

嗯，你们不需要现在就知道这个过程的细节。

Uh, you don't need to know the details of the process right now.

We are still figuring out just how it works ourselves.

但是你应该会对矿物进化这个概念怎么用在寻找其它星球的生命证据上面感兴趣。

But you might be interested to know that this concept of mineral evolution is being used in the search for evidence of life on other planets.

我们的想法是，如果一些矿物质在地球上产生了，是作为生物活动过程的结果产生的，并且如果我们在其他星球上也发现了这些矿物质，这就可以说明生命曾经在那里存在过！

The thinking is that if certain minerals occur here on Earth, as a result of a biological process, and if we also find those same minerals on another planet, this would suggest that life may have once existed there!

但是就是因为我们在火星上或者金星上找到了某种特定的矿物质，我们真的不应该假定，发生在地球上的过程也会在那里发生，也不应该假定在它们上面产生矿物质的过程和地球上的一样。

But just because a particular mineral is found on, say Mars or Venus, we really shouldn't assume that whatever caused it to turn up there, must be the same process that formed that mineral here on Earth.

What point does the professor make about the minerals present during Earth's formation?

What similarities does the professor point out between minerals and living organisms?

Why does the professor talk about microbial mats?

What does the professor think about using evidence of minerals on another planet to determine whether life has existed there?

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