Changes in atmospheric carbon dioxide (CO2) concentration directly influence the ratio of stomatal water loss to carbon uptake. This ratio (e) is a fundamental quantity for terrestrial ecosystems, as it defines the water requirement for plant growth. Statistical and analogue-based methods used to reconstruct past hydroclimate variables from fossil pollen assemblages do not take account of the effect of CO2 variations on e. Here we present a general, globally applicable method to correct for this effect. The method involves solving an equation that relates e to a climatic moisture index (MI, the ratio of mean annual precipitation to mean annual potential evapotranspiration), mean growing-season temperature, and ambient CO2. The equation is b...
The best records of atmospheric change of glacial cycles are those from ice cores. However, ice core...
We describe a new method for making palaeoclimate reconstructions. The method produces seasonal pala...
Atmospheric [CO2] over the past 800 000 yr has varied generally as a function of glacial periods, wi...
We present a novel method to quantify the ecophysiological effects of changes in CO2 concentration d...
We present a novel method to quantify the ecophysiological effects of changes in CO2 concentration d...
We present a novel method to quantify the ecophysiological effects of changes in CO2 concentration d...
We present a novel method to quantify the ecophysiological effects of changes in CO₂ concentration d...
Plant water-use efficiency (WUE), which is the ratio of the uptake of carbon dioxide through photosy...
Isotopic measurements on junipers growing in southern California during the last glacial, when the a...
Isotopic measurements on junipers growing in southern California during the last glacial, when the a...
Subfossil pollen and plant macrofossil data derived from C-14-dated sediment profiles can provide qu...
This is the final version of the article. Available from the European Geosciences Union (EGU) via th...
Atmospheric CO2 concentration has greatly fluctuated during the Quaternary. These variations have in...
Increases in atmospheric [CO2] (CO2 concentration) over the last several hundred years have resulted...
Increases in atmospheric [CO2] (CO2 concentration) over the last several hundred years have resulted...
The best records of atmospheric change of glacial cycles are those from ice cores. However, ice core...
We describe a new method for making palaeoclimate reconstructions. The method produces seasonal pala...
Atmospheric [CO2] over the past 800 000 yr has varied generally as a function of glacial periods, wi...
We present a novel method to quantify the ecophysiological effects of changes in CO2 concentration d...
We present a novel method to quantify the ecophysiological effects of changes in CO2 concentration d...
We present a novel method to quantify the ecophysiological effects of changes in CO2 concentration d...
We present a novel method to quantify the ecophysiological effects of changes in CO₂ concentration d...
Plant water-use efficiency (WUE), which is the ratio of the uptake of carbon dioxide through photosy...
Isotopic measurements on junipers growing in southern California during the last glacial, when the a...
Isotopic measurements on junipers growing in southern California during the last glacial, when the a...
Subfossil pollen and plant macrofossil data derived from C-14-dated sediment profiles can provide qu...
This is the final version of the article. Available from the European Geosciences Union (EGU) via th...
Atmospheric CO2 concentration has greatly fluctuated during the Quaternary. These variations have in...
Increases in atmospheric [CO2] (CO2 concentration) over the last several hundred years have resulted...
Increases in atmospheric [CO2] (CO2 concentration) over the last several hundred years have resulted...
The best records of atmospheric change of glacial cycles are those from ice cores. However, ice core...
We describe a new method for making palaeoclimate reconstructions. The method produces seasonal pala...
Atmospheric [CO2] over the past 800 000 yr has varied generally as a function of glacial periods, wi...