Objective: To evaluate the cardiopulmonary effects of open sea scuba air diving to 39 m (30 minutes bottom time) with standard decompression. To account for possible gravity dependent effects of venous gas bubbles, the variables were measured in different post-dive body postures and compared with the baseline values before the dive in the same posture. Methods: Eight male divers conducted two similar dives on successive days. Their posture before and after the dive was either sitting or supine, in random order. The divers were evaluated before and 30, 60, and 90 minutes after the dive. Venous bubbles were detected by precordial Doppler after the dive in four divers in the supine posture and two divers in the sitting posture. Results: Arterialised oxygen tension had decreased at all times after the dive (211.3 mm Hg, p = 0.00006), due to decreased alveolar oxygen tension, irrespective of posture. Apart from an increase in the sitting posture 30 minutes after the dive, pulmonary capacity for carbon monoxide diffusion and cardiac index decreased, mostly 60 minutes after the dive (29%, p = 0.0003 and 220%, p = 0.0002 respectively). The decrease in cardiac index was greater in the supine posture (p = 0.0004), and the physiological dead space/tidal volume ratio increased more in the sitting position (p = 0.006). Conclusions: Field dives are associated with moderate impairments in cardiac output and gas exchange. Some of these impairments appear to depend on the posture of the diver after the dive. W e have previously reported that air dry dives to 45 m (25 minutes bottom time) are associated with acute, transient reductions in pulmonary diffusing capacity for CO (CO transfer factor (TLCO)) and arterial oxygen saturation (SaO 2 ).1 The maximal decrease in TLCO was 15% 40 minutes after the dive. Thorsen et al 2 confirmed these results, reporting, however, smaller TLCO reductions after a dry dive to 39 m. A later study observed post-dive decreases in dynamic lung flows and volumes.3 Both dry and wet (open sea) dives are associated with hyperoxia, increased density of breathing gas, and decompression stress with possible formation of venous bubbles and subsequent lung microembolisation (venous gas microemboli (VGM)). However, in open sea bounce dives there is also immersion, the mechanical load of the breathing apparatus, a greater level of physical activity, and exposure to a cold environment. Immersion in cold seawater results in breathing of colder and denser gas and may also, by inducing peripheral cutaneous vasoconstriction in conjunction with the immersion effect, potentiate greater central pooling of blood than in dry dives. Most previous studies on pulmonary function after open sea dives investigated professional, saturation dives, 2 4-7 focusing on the effects observed days, weeks, and years after the dives. In contrast, Skogstad et al 8 measured pulmonary function two hours after open sea bounce air dives to 10 and 50 m. They reported similar reductions in TLCO (11-13%) in both dives, in conjunction with spirome...