On Earth, nearly all iron ore comes from specific rocks called banded iron formations, the vast majority of which originate around 2,000 million years ago (2,400-1,800 Mya to be more precise). At this time, the world’s oceans were far more acidic, able to dissolve iron minerals. The acidity arose due to the large amount of carbon dioxide in the atmosphere that dissolved in the oceans to form carbonic acid. Around 2,000 million years ago, there was no breathable oxygen on Earth’s surface. But then, a cellular mutation allowed certain bacteria to breathe in carbon dioxide and breathe out oxygen – the birth of photosynthesis. The new bacteria thrived. As they pumped oxygen into the oceans, it bonded with the iron minerals that then precipitated as solid sediments onto the ocean floor. For reasons still being investigated by earth scientists, the available oxygen fluctuated through time. When there was an abundance of oxygen, the ocean sediments became rich with iron-oxide minerals. When there was a dearth of oxygen, the ocean sediments returned to their anoxic, muddy state (forming chert). This cycle repeated for 100s of millions of years, creating alternating bands of rock, some with precipitated iron, some without: the banded iron formations. If Westeros has followed a similar geologic evolution as Earth, then the Iron Islands record the birth of breathable air on the Game of Thrones planet.
Scars of the past: Students explore agriculture and human conflict in Cambodia
Beneath Cambodia’s troubled history with the Khmer Rouge lies a complex agricultural legacy that reaches back centuries. A group of Stanford students traveled to Cambodia with Earth science and mental health experts to explore the ways food, water, and human conflict have shaped the country.
That’s No Moon…
Scientists use DNA to investigate cleaner energy sources
Stanford researchers found that DNA-embedded nanoparticles can survive the harsh environments of geothermal energy systems, allowing for better mapping of cleaner energy sources.
A Student of ‘Cultural Environmentalism’ Explores the Many Views of Earth’s Anthropocene ‘Age of Us’
A Stanford University team has boldly proposed that – living as we are through the last years of one Earth epoch, and the birth of another – we belong to “Generation Anthropocene”