Researchers have figured out how to use mineral-rich deposits in caves known as speleothems as proxies for prehistoric climates. Speleothems form layers that grow during wet periods and form dusty skins when the water dries up.
Scientists can date the layers with extreme precision based on the radioactive decay of uranium into its daughter product thorium. Variations in their thickness is determined by a combination of the amount of water seeping into the cave and the concentration of carbon dioxide in the cave’s atmosphere.
When conditions are right, the layers provide a measure of how the amount of precipitation above the cave varies over time.
Analyzing the ratios of heavy to light isotopes of oxygen present in the layers allows researchers to track changes in the temperature at which the water originally condensed into droplets in the atmosphere and whether the rainfall’s point of origin was local or if traveled a long way before falling to the ground.
The value of this information is illustrated in a new study published in Geophysical Research Letters in which researchers made a detailed record of the last 50 years of growth of a stalagmite that formed in Mawmluh Cave in the East Khasi Hills district in the northeastern Indian state of Meghalaya, an area credited as the rainiest place on Earth.
Studies of historical records in India suggest that reduced monsoon rainfall in central India has occurred when the sea surface temperatures in specific regions of the Pacific Ocean were warmer than normal. These naturally recurring sea surface temperature “anomalies” are known as the El Niño Modoki, which occurs in the central Pacific, and the Pacific Decadal Oscillation, which takes place in the northern Pacific. By contrast, the historical record indicates the traditional El Niño, which occurs in the eastern Pacific, has little effect on rainfall levels in the subcontinent.
When researchers analyzed the Mawmluh stalagmite record, the results were consistent with the historical record. Specifically, they found that during El Niño Modoki events, when drought was occurring in central India, the mineral chemistry suggested more localized storm events occurred above the cave, while during the non-El Niño periods, the water that seeped into the cave had traveled much farther before it fell, which is the typical monsoon pattern.
“Now that we have shown that the Mawmluh cave record agrees with the instrumental record for the last 50 years, we hope to use it to investigate relationships between the Indian monsoon and El Niño during prehistoric times such as the Holocene,” says Jessica Oster, assistant professor of earth and environmental sciences at Vanderbilt University.
The Holocene Climate Optimum was a period of global climate warming that occurred between six to nine thousand years ago. At that time, the global average temperatures were somewhere between four to six degrees Celsius higher than they are today. That is the range of warming that climatologists are predicting due to the build-up of greenhouse gases in the atmosphere from human activity.
So information about the behavior of the monsoon during the Holocene could provide clues to how it is likely to behave in the future. This knowledge could be very important for the 600 million people living on the Indian subcontinent who rely on the monsoon, which provides the area with 75 percent of its annual rainfall.
“The study actually grew out of an accidental discovery,” Oster says.
Vanderbilt graduate student Chris Myers visited the cave, which coauthor Sebastian Breitenbach from the University of Cambridge has been studying for several years, to see if it contained enough broken speleothems to date major prehistoric earthquakes in the area.
Myers found a number of columns that appeared to have broken off in the magnitude 8.6 earthquake that hit Assam, Tibet, in 1950. But he also discovered a number of new stalagmites that had begun growing on the broken bases. When he examined these in detail, he found they had very thick layers and high concentrates of uranium, which made them perfect for analysis.
Because of the large amount of water running into the cave, the stalagmite they choose to analyze had grown about 2.5 centimeters in 50 years. (If that seems slow, compare it with growth rates of a few millimeters in a thousand years found in caves in arid regions like the Sierra Nevada.) As a result, the annual layers averaged about 0.4 millimeters thick—wide enough for the researchers to get seven to eight samples per layer, which is slightly better than one measurement every two months.
The amount of information about the climate that scientists can extract from the stalagmites and stalactites in a cave is amazing. But the value of this approach increases substantially as the number of caves that can act as climate proxies increases.
It is not a simple task. Because each cave is unique, scientists have to study it for several years before they understand it well enough to use it as a proxy. For example, they must establish how long it takes water to move from the surface down to the cave, a factor that can vary from days to months.
Other researchers from Vanderbilt and from the Smithsonian National Museum of Natural History contributed to the study. The Vanderbilt International Office, the National Science Foundation, the Cave Research Foundation, the Geological Society of America, and the Swiss National Science Foundation funded the work.
Source: Vanderbilt University