This chapter discusses the carbon dioxide assimilation in plants. All oxygenic (oxygen-evolving) organisms from the simplest prokaryotic cyanobacteria to the most complicated land plants have a common pathway for the reduction of CO2 to sugar phosphates. This pathway is known as the reductive pentose phosphate (RPP), Calvin-Benson or C3 cycle. Although the RPP cycle is the fundamental carboxylating mechanism, a number of plants have evolved adaptations in which CO2 is first fixed by a supplementary pathway and then released in the cells in which the RPP cycle operates. One of these supplementary pathways, the C4 pathway, involves special leaf anatomy and a division of biochemical labor between cell types. Plants endowed with this pathway, through greater efficiency, are able to flourish under conditions of high light intensity and elevated temperatures. A second supplementary pathway was first found in species of the Crassulaceae and is called Crassulacean acid metabolism (CAM). These plants are often found in dry areas and fix CO2 at night into C4 acids. During the day, the leaves can close their stomata to conserve water, while CO2 released from the C4 acids is converted to sugar phosphates by the RPP cycle using absorbed light energy. CO2 fixation is also found in many bacteria, both photosynthetic and non-photosynthetic. The purple sulfur and purple nonsulfur bacteria employ the RPP cycle as do plants. The photosynthetic green bacteria, however, use a group of ferredoxin-linked carboxylases in a pathway known as the reductive carboxylic acid cycle.