Climatic changes must have greatly affected the distribution of malaria in prehistoric times. Paleobotanical evidence, snowline depression studies and information obtained from deep sea sediment cores, indicate that southern Europe must have suffered a drop of summer temperatures of approximately 9 degrees C during the last glacial maximum, 18,000 years ago. Such a drop would have been decisive as regards the distribution of malaria and its vectors. If present at all, the disease would have been confined to the southernmost parts of the continent but P. falciparum and today's most effective vectors--A. labranchiae and A. sacharovi--would have been excluded from Europe. In western Asia, summer temperatures 6 degrees C lower than those of today would have had less effect on the malaria situation. The introduction of falciparum malaria in southern Europe is placed in Hellenistic and Early Imperial Roman times, based on paleoclimatological evidence and historical and medical data. In America P. falciparum is also considered a late entrant but vivax and quartan malaria may have been introduced in pre-Columbian times. In the Pacific, the disease is known to have been spread by man since the Age of Discovery until contemporary times.