Despite the abundance of oxygen in atmospheric air relative to water, the initial loss of respiratory surface area and accumulation of carbon dioxide in the blood of amphibious fishes during emersion may result in hypoxemia. Given that the ability to respond to low oxygen conditions predates the vertebrate invasion of land, we hypothesized that amphibious fishes maintain O 2 uptake and transport while emersed by mounting a co-opted hypoxia response. We acclimated the amphibious fish Kryptolebias marmoratus, which are able to remain active for weeks in both air and water, for 7 days to normoxic brackish water (15‰, ~21 kPa O 2 ; control), aquatic hypoxia (~3.6 kPa), normoxic air (~21 kPa) or aerial hypoxia (~13.6 kPa). Angiogenesis in the skin and bucco-opercular chamber was pronounced in air-versus water-acclimated fish, but not in response to hypoxia. Aquatic hypoxia increased the O 2 -carrying capacity of blood via a large (40%) increase in red blood cell density and a small increase in the affinity of hemoglobin for O 2 (P 50 decreased 11%). In contrast, air exposure increased the hemoglobin O 2 affinity (decreased P 50 ) by 25% without affecting the number of red blood cells. Acclimation to aerial hypoxia both increased the O 2 -carrying capacity and decreased the hemoglobin O 2 affinity . These results suggest that O 2 transport is regulated both by O 2 availability and also, independently, by air exposure. The ability of the hematological system to respond to air exposure independent of O 2 availability may allow extant amphibious fishes, and may also have allowed primitive tetrapods to cope with the complex challenges of aerial respiration during the invasion of land.KEY WORDS: Hemoglobin, Oxygen-carrying capacity, Hemoglobin-oxygen affinity, Air-breathing organ, Air-breathing fish, Mangrove rivulus
INTRODUCTIONThe transition from aquatic to terrestrial life represents a major step in vertebrate evolution because the physical conditions between these environments are dramatically different. Oxygen solubility is relatively low in water and even well-oxygenated aquatic environments contain only about 3% of the O 2 available in atmospheric air (Dejours, 1988). Low concentrations of aquatic O 2 , particularly in hypoxic habitats, have often been hypothesized to be one of the driving forces behind the evolution of amphibious or terrestrial life histories because invasion of land would allow animals to exploit the O 2 -rich aerial environment (Graham, 1997).
RESEARCH ARTICLEDepartment of Integrative Biology, University of Guelph, Guelph, ON N1G 2W1, Canada.*Author for correspondence (aturko@uoguelph.ca)
Received 4 July 2014; Accepted 15 September 2014Taking advantage of aerial O 2 presents several challenges for fishes. Water-breathing fishes exchange respiratory gases across the gills but during emersion the gill lamellae typically collapse and coalesce, reducing the surface area available for respiration. Accumulation of CO 2 in the blood of emersed fishes, resulting from the low solubility of CO 2 in...