Tibet sediments reveal climate patterns from late Miocene, six million years ago

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The Tibetan Plateau in China experiences the strongest monsoon system on Earth, with powerful winds—and accompanying intense rains in the summer months—caused by a complex system of global air circulation patterns and differences in surface temperatures between land and oceans.

Tibet sediments reveal climate patterns from late Miocene, six million years ago
Stratification in Tibet sediment. Climate variations are reflected in color variations with the red sediment typically
 indicating a wetter climate and the white indicating a drier climate. “You can literally walk up time 
as you sample the sediment,” Garzione says [Credit: Qingquan Meng]

These extreme weather patterns make this area an ideal location for climate scientists to study the delicate interconnected web of the global climate system.

Carmala Garzione, a professor of earth and environmental sciences at the University of Rochester, and Junsheng Nie, a visiting research associate at the University, surveyed sediment samples from the northern Tibetan Plateau’s Qaidam Basin and were able to construct paleoclimate cycle records from the late Miocene epoch of Earth’s history, which lasted from approximately 11 to 5.3 million years ago. They recently published their findings in Science Advances.

Reconstructing past climate records can help scientists determine both natural patterns and the ways in which future glacial events and greenhouse gas emissions may affect global systems.

Based on previous research on ice core, marine, and sediment records, researchers determined that for the past 800,000 years, Northern Hemisphere ice ages—in which vast areas of North America, Europe, and Asia are covered with thick sheets of ice—occurred about every 100,000 years. Prior to that period, ice ages occurred more frequently, on cycles of 41,000 years, and scientists believed this was the norm.

Using the sediment samples from the Qaidam Basin, Nie and Garzione show that the East Asian monsoon patterns in the late Miocene also follow similar 100,000 year cycles, with stronger monsoons peaking at 100,000 years and diminishing in the periods in between. This reveals a greater than 6 million earlier onset of these 100,000 year cycles than was previously documented.

“People have been thinking that the 100,000 year cycle was a later Quaternary [present-day] climate anomaly,” Nie says. “But from our results, we see that it’s not an anomaly, it was present many years before.”

Several factors affect these cycles, but they are ultimately determined by orbital forcing—the Sun’s radiation received by the Earth due to variations in the Earth’s orbit in the solar system. There are three types of variations that occur simultaneously, known as the Milankovitch Cycles:

  1. Eccentricity: How the Earth rotates around the Sun—the shape of Earth’s orbit gradually changes from being more oval to more round over a period of 100,000 years.
  2. Axial tilt: The Earth tilts toward the Sun at an angle that changes from an approximate 22-degree tilt to a 24.5-degree tilt over a period of 41,000 years.
  3. Precession of equinox: The Earth slowly wobbles as it spins, much like a toy top, while at the same time, the Earth’s rotational axis—the line from the north to south poles—rotates. The interaction of these two processes results in cyclical movement of equinoxes over a period of approximately 23,000 years.

“Each of these factors influences incoming solar radiation and how the earth is absorbing heat,”Garzione says.

Mysteries remain because eccentricity is the weakest cycle, so should logically not be the dominant cycle for climatic events. It is not only sunlight that plays a role in these cycles, but the influence of glaciers and atmospheric carbon dioxide.

For the past one million years, the waxing and waning of Northern Hemisphere ice sheets—mainly those in Canada—have controlled the climate cycles, by affecting ocean currents, temperatures, and wind patterns. Southern Hemisphere ice in Antarctica has remained relatively fixed, without any major glacial melting to catalyze advances and retreats.

During the late Miocene, this was the opposite, with ice in Antarctica in the Southern Hemisphere waxing and waning. Nie and Garzione suggest that the fluctuating Antarctic ice sheet in the late Miocene, at a time when there was minimal ice in the Northern Hemisphere, exerted the dominant control on the 100,000 year cycles observed in the Qaidam Basin record.

“If one hemisphere sees major advances and retreats in ice sheets, that’s when we get into this pattern of 100,000 year cycles dominating,” Garzione says. “The question is, will we push carbon dioxide high enough in the future that the Northern Hemisphere remains ice free and the advances and retreats begin again with the Southern Hemisphere ice sheets.”

If so, the Southern Hemisphere ice sheets may once again exert dominant influence on climate cycles.

Source: University of Rochester [April 06, 2017]

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