Himalayan deposits reveal ancient ocean water, linking glaciation to Earth’s oxygenation and life evolution.
High up in the Himalayas, researchers from the Indian Institute of Science (IISc) and Niigata University in Japan have found water droplets trapped in mineral deposits, likely remnants from an ancient ocean that existed approximately 600 million years ago. Through an examination of the deposits, containing both calcium and magnesium carbonates, the team was able to propose a potential explanation for occurrences that might have led to a major oxygenation event in Earth’s history.
“We have found a time capsule for paleo oceans,” says Prakash Chandra Arya, a Ph.D. student at the Centre for Earth Sciences (CEaS), IISc, and first author of the study published in Precambrian Research.
The Connection Between Snowball Earth and Oxygenation Events
Scientists believe that between 700 and 500 million years ago, thick sheets of ice covered the Earth for an extended period, called the Snowball Earth glaciation (one of the major glacial events in Earth’s history). What followed this was an increase in the amount of oxygen in the Earth’s atmosphere, called the Second Great Oxygenation Event, which eventually led to the evolution of complex life forms. So far, scientists have not fully understood how these events were connected due to the lack of well-preserved fossils and the disappearance of all past oceans that existed in the Earth’s history. Exposures of such marine rocks in the Himalayas can provide some answers.
“We don’t know much about past oceans,” says Prakash. “How different or similar were they compared to present-day oceans? Were they more acidic or basic, nutrient-rich or deficient, warm or cold, and what was their chemical and isotopic composition?” Such insights could also provide clues about the Earth’s past climate, and this information can be useful for climate modeling, he adds.
The deposits found by the team – which date back to around the time of the Snowball Earth glaciation – showed that the sedimentary basins were deprived of calcium for an extended period, probably due to low riverine input. “During this time, there was no flow in the oceans, and hence no calcium input. When there is no flow or calcium input, as more calcium precipitates, the amount of magnesium goes up,” explains Sajeev Krishnan, Professor at CEaS and corresponding author of the study. The magnesium deposits formed at this time were able to trap paleo ocean water in their pore space as they crystallized, the researchers suggest.
The calcium deprivation also likely led to a nutrient deficiency, making it conducive for slow-growing photosynthetic cyanobacteria, which could have started spewing out more oxygen into the atmosphere. “Whenever there is an increase in the oxygen level in the atmosphere, you will have biological radiation (evolution),” says Prakash.
Tracing Oceanic Evolution Through Himalayan Deposits
The team hunted for these deposits across a long stretch of the western Kumaon Himalayas, extending from Amritpur to the Milam glacier, and Dehradun to the Gangotri glacier region. Using extensive laboratory analysis, they were able to confirm that the deposits are a product of precipitation from ancient ocean water, and not from other places, such as the Earth’s interior (for example, from submarine volcanic activity).
The researchers believe that these deposits can provide information about ancient oceanic conditions such as pH, chemistry, and isotopic composition, which have so far only been theorized or modeled. Such information can help answer questions related to the evolution of oceans, and even life, in Earth’s history.
Reference: “Himalayan magnesite records abrupt cyanobacterial growth that plausibly triggered the Neoproterozoic Oxygenation Event” by Prakash Chandra Arya, Claude Nambaje, S. Kiran, M. Satish-Kumar and K. Sajeev, 17 July 2023, Precambrian Research.
DOI: 10.1016/j.precamres.2023.107129
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