Oxygen-18 of O2 Records the Impact of Abrupt Climate Change on the Terrestrial Biosphere

Photosynthesis and respiration occur widely on Earth's surface, and the O-18/O-16 ratio of the oxygen produced and consumed varies with climatic conditions. As a consequence, the history of climate is reflected in the deviation of the O-18/O-16 of air (delta O-18(atm)) from seawater delta O-18 (known as the Dole effect). We report variations in delta O-18(atm) over the past 60,000 years related to Heinrich and Dansgaard-Oeschger events, two modes of abrupt climate change observed during the last ice age. Correlations with cave records support the hypothesis that the Dole effect is primarily governed by the strength of the Asian and North African monsoons and confirm that widespread changes in low-latitude terrestrial rainfall accompanied abrupt climate change. The rapid delta O-18(atm) changes can also be used to synchronize ice records by providing global time markers.