High-resolution carbon dioxide concentration record 650,000-800,000 years before present.

Changes in past atmospheric carbon dioxide concentrations can be determined by measuring the composition of air trapped in ice cores from Antarctica. So far, the Antarctic Vostok and EPICA Dome C ice cores have provided a composite record of atmospheric carbon dioxide levels over the past 650,000 years. Here we present results of the lowest 200 m of the Dome C ice core, extending the record of atmospheric carbon dioxide concentration by two complete glacial cycles to 800,000 yr before present.

Stable carbon cycle-climate relationship during the Late Pleistocene.

A record of atmospheric carbon dioxide (CO2) concentrations measured on the EPICA (European Project for Ice Coring in Antarctica) Dome Concordia ice core extends the Vostok CO2 record back to 650,000 years before the present (yr B.P.).

Eight glacial cycles from an Antarctic ice core.

The Antarctic Vostok ice core provided compelling evidence of the nature of climate, and of climate feedbacks, over the past 420,000 years. Marine records suggest that the amplitude of climate variability was smaller before that time, but such records are often poorly resolved. Moreover, it is not possible to infer the abundance of greenhouse gases in the atmosphere from marine records.

The influence of ozone and nutrition on δC in Betula pendula.

In the cellulose of stems and leaves, δC was investigated in a birch clone (Betula pendula), which was exposed throughout the growing season to either <3 (control) or 90/40 nl O 1 (day/night). Each regime was split into plants under high or low nutrient supply. δC was increased (becoming less negative), in stems rather than leaves, by both high nutrition (+2‰) and O stress (+1‰).

Influence of Ozone on the Stable Carbon Isotope Composition, deltaC, of Leaves and Grain of Spring Wheat (Triticum aestivum L.).

The relative composition of stable carbon isotopes, delta(13)C, was determined in flag leaves and grain of spring wheat (Triticum aestivum L. cv Albis) grown in open-top field fumigation chambers and exposed to different O(3) levels during the growing season. The aim of the study was to establish exposure-response relationships for the radiation-weighted seasonal mean O(3) concentration and delta(13)C (relative deviation of the (13)C/(12)C ratio) values of the two plant parts.