Mashable 2024年11月16日
Scientists find evidence that entirety of Earth was once covered in ice
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一项新的研究表明,大约7.2亿至6.35亿年前,地球经历了一次严重的冰河时期,被称为“雪球地球”。研究人员在科罗拉多州发现了证据,表明即使是热带地区也曾被厚厚的冰川覆盖。这挑战了之前的一些观点,即在“雪球地球”时期,一些海洋和陆地可能未被冰雪完全覆盖。研究团队通过对塔瓦砂岩的分析,发现其特征与南极洲冰盖下的砂岩相似,并利用铀衰变测年法确定了其形成时间,与“雪球地球”时期相吻合。这项研究为理解史前冰河时期的程度提供了新的线索,也提醒我们地球环境的巨大变化能力。

❄️ **科罗拉多州塔瓦砂岩的发现为‘雪球地球’理论提供了新的证据:**研究人员在科罗拉多州的落基山脉发现了塔瓦砂岩,其特征与现代冰盖下的砂岩相似,表明该地区在‘雪球地球’时期可能被冰川覆盖。

📅 **铀衰变测年法确定了塔瓦砂岩的形成时间,与‘雪球地球’时期相吻合:**通过对塔瓦砂岩中矿脉的铀衰变测年,研究人员确定其形成时间与7.2亿至6.35亿年前的‘雪球地球’时期一致,进一步支持了冰川覆盖热带地区的假设。

🌡️ **温室气体减少可能是导致‘雪球地球’形成的原因:**科学家认为,地球上温室气体(如二氧化碳)的大幅减少,可能导致全球气温骤降,最终引发了“雪球地球”事件。

🌍 **‘雪球地球’事件的结束可能与小行星撞击有关:**一些研究表明,“雪球地球”事件的结束可能与一次大型小行星撞击有关,撞击产生的热量和气体导致冰川融化,地球逐渐恢复到正常状态。

🗺️ **更多研究将有助于揭示‘雪球地球’的完整图景:**目前的研究仅针对科罗拉多州的一个区域,未来需要更多研究来全面了解“雪球地球”时期冰川覆盖的范围和程度。

Even the balmy tropics may have once been crushed by colossal masses of ice.

A severe ice age dominated Earth, some 720 to 635 million years ago, well before dinosaurs stalked the land. But it's uncertain if the entire world froze over during the glaciations of this long-lived, extreme episode, dubbed "Snowball Earth." Now, new evidence from Colorado, an area that once was located in the tropics, suggests mighty glaciers sprawled over even Earth's warmest regions.

"This study presents the first physical evidence that Snowball Earth reached the heart of continents at the equator," Liam Courtney-Davies, a geologist at CU Boulder who led the new research, said in a statement. The research was recently published in Proceedings of the National Academy of Sciences, a leading science journal.

A dramatic decrease in greenhouse gases that trap heat on the globe — notably carbon dioxide — may have triggered the slide into a frozen orb. Previous research has suggested that even though Earth's average temperature dropped well below freezing, some of the ocean surface and land resisted turning to or getting blanketed in thick, hard ice.

But evidence in the lofty Colorado mountains points to heavy ice in the tropics.

The telltale rocks are called Tava sandstone, which are exposed in the Rocky Mountains. As you might have guessed, sandstone started out as sand on the surface, but is compacted together by different activities, such as grains in rivers becoming buried by layers and layers of silt. In this case, the researchers say the Tava sandstone resembles the type of features found underneath ice sheets, like those in present-day Antarctica.

To see if heavy glaciers may have compacted this once-tropical sandstone (shown below), the researchers dated the mineral veins that crossed through the sandstone. They shot these ancient, rusted minerals with a laser, which discharged uranium, a common radioactive element in Earth's crust. Crucially, uranium naturally decays at a constant rate, providing a dating technique and a good idea of when something formed.

Orangish Tava sandstone exposed atop the Rocky Mountains. Credit: Christine Siddoway / CU Boulder
The dark reddish-brown bands are the layers of Tava sandstone researchers say were crushed under heavy glaciers during Snowball Earth. Credit: Liam Courtney-Davies / CU Boulder

The result? The uranium dating lines up with the period of Snowball Earth, hundreds of millions of years ago.

This is a compelling find, suggesting great glaciers compressed a once tropical Colorado. But this is just one surveyed area. More surveys are needed to truly grasp the extent of this vast ice cover on Earth. 

"We want to get the word out so that others try and find these features and help us build a more complete picture of Snowball Earth,” Courtney-Davies said.

Eventually, the extreme ice age ended, perhaps stoked by a massive asteroid strike that blew a plethora of heat trapping gasses into the atmosphere, melting the ice and forcing weighty glaciers to retreat. Earth's crust continues to reveal our planet's wild ride over billions of years — a ride that continues today on Earth's ever-moving surface.

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雪球地球 冰河时期 地质学 古气候 塔瓦砂岩
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