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Haemolymph oxygen transport and acid-base status in Glyptonotus antarcticus Eights
Authors:N. M. Whiteley  E. W. Taylor  A. Clarke  A. J. El Haj
Affiliation:(1) School of Biological Sciences, University of Birmingham, Birmingham B15 2TT, UK fax: 0121 414 5925; e-mail: whitelnm@novell2.bham.ac.uk, GB;(2) British Antarctic Survey, High Cross, Madingley Road, Cambridge CB3 OET, UK, GB
Abstract:Haemolymph samples were withdrawn from routinely active male intermoult Glyptonotus held at 0 ± 0.5°C, and analysed for blood-gas and acid-base variables. In both the arterialised (a) and venous (v) haemolymph, over 50% of the oxygen was transported as dissolved oxygen at PaO2 and PvO2 levels of 12.0 ± 1.15 and 7.70 ± 1.89 kPa, respectively. The maximum oxygen-carrying capacity of the haemocyanin (CmaxHcO2) was relatively low at 0.19 ± 0.05 mmol l−1, accompanied by relatively low protein and [Cu2+] levels indicating low circulating haemocyanin concentrations. Arterialised haemolymph had a mean pH of 7.88 ± 0.02(6) at a PCO2 of 0.12 ± 0.01(6) kPa and a bicarbonate level of 12.95 ± 0.80(6) mequiv l−1 with small differences in PCO2 and pH between arterial and venous haemolymph. The non-bicarbonate buffering capacity of Glyptonotus haemolymph was low at −2.0 mequiv l−1 HCO3 pH unit−1. Haemolymph [l-lactate] and [d-glucose] levels were similar at < 1 mmol l−1 in animals held in the laboratory and those sampled in Antarctica. The blood-gas and acid-base status of Glyptonotus haemolymph may be a reflection of the low and stable temperatures experienced by this Antarctic crustacean. Received: 14 August 1996 / Accepted: 3 November 1996
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