In an analysis of the past 1.2 million years, UC Santa Barbara geologist¹ Lorraine Lisiecki discovered a pattern that connects the regular changes of the Earth's orbital（轨道的，眼窝的） cycle to changes in the Earth's climate. The finding is reported in this week's issue of the scientific journal Nature Geoscience. Lisiecki performed her analysis of climate by examining ocean sediment²（沉淀物，沉积） cores. These cores come from 57 locations around the world. By analyzing³ sediments⁴, scientists are able to chart the Earth's climate for millions of years in the past. Lisiecki's contribution is the linking of the climate record to the history of the Earth's orbit.

It is known that the Earth's orbit around the sun changes shape every 100,000 years. The orbit becomes either more round or more elliptical（椭圆的，省略的） at these intervals⁵（间隔） . The shape of the orbit is known as its "eccentricity⁶（离心率，古怪） ." A related aspect is the 41,000-year cycle in the tilt⁷（倾斜） of the Earth's axis⁸（轴，轴线） .

Glaciation（冰川作用） of the Earth also occurs every 100,000 years. Lisiecki found that the timing⁹ of changes in climate and eccentricity coincided. "The clear correlation¹⁰（相关，关联） between the timing of the change in orbit and the change in the Earth's climate is strong evidence of a link between the two," said Lisiecki. "It is unlikely that these events would not be related to one another."

Besides finding a link between change in the shape of the orbit and the onset¹¹ of glaciation, Lisiecki found a surprising correlation. She discovered that the largest glacial cycles occurred during the weakest changes in the eccentricity of Earth's orbit –– and vice¹² versa（反之亦然） . She found that the stronger changes in the Earth's orbit correlated to weaker changes in climate. "This may mean that the Earth's climate has internal instability in addition to sensitivity to changes in the orbit," said Lisiecki.

She concludes that the pattern of climate change over the past million years likely involves complicated interactions（相互作用） between different parts of the climate system, as well as three different orbital systems. The first two orbital systems are the orbit's eccentricity, and tilt. The third is "precession," or a change in the orientation¹³（方向，定向） of the rotation¹⁴ axis.