Phosphonate metabolism of Trichodesmium IMS101 and the production of greenhouse gases

Abstract

A series of laboratory experiments were conducted to investigate (1) the capacity of Trichodesmium IMS101 to hydrolyze phosphonates as a source of phosphorus (P) for growth, (2) the stoichiometric relationship between phosphonate use and biogenic gas production, and (3) the potential inhibition of phosphonate hydrolysis by additions of dissolved inorganic phosphorus (DIP). Trichodesmium IMS101 is capable of cleaving the carbon-P bond found in methylphosphonate (MPn) and ethylphosphonate (EPn), and the decomposition of these particular phosphonates results in the stoichiometric production of the greenhouse gases methane (CH4) and ethane (C2H 6), respectively. Growth on 2-aminoethylphosphonate (2-AEP) led to modest ethylene (C2H4) production. Normalized to rates of Trichodesmium carbon (C) fixation, biogenic gas production as a result of either MPn or EPn hydrolysis (0.95 ± 0.04 mmol CH4 (mol C) -1 and 1.18 ± 0.11 mmol C2H6 (mol C)-1, respectively) approximates rates of DIP use (1.11 ± 0.05 P mmol P (mol C)-1) measured in parallel cultures. DIP, MPn, and EPn can be used by Trichodesmium IMS101 as a sole source of P with equal metabolic efficiency. Additionally, neither MPn hydrolysis nor the production of CH 2 was significantly inhibited by additions of up to 30 μmol DIP L-1. These results imply that Trichodesmium can use multiple P resources simultaneously for growth and that the production of greenhouse gases occurs during decomposition pathways of select phosphonates. © 2010, by the American Society of Limnology and Oceanography, Inc.