Kinetic isotope effect and characterization of form II RubisCO from the chemoautotrophic endosymbionts of the hydrothermal vent tubeworm Riftia pachyptila

By J. Robinson, Kathleen M. Scott, S. T. Swanson, Marion H. O'Leary, K. Horken, F. R. Tabita, Colleen M. Cavanaugh. 2003

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Marine Chemosynthetic Symbioses (2006, background): “…Goericke et al., 1994), carbon derived chemosynthetically at vents is either considerably lighter (enriched in 12C), with δ13C values from µ27‰ to µ35‰, or heavier (depleted in 12C), with values from µ9‰ to µ16‰ (Childress and Fisher, 1992; Robinson and Cavanaugh, 1995; Robinson et al., 2003).”
The age of Rubisco: the evolution of oxygenic photosynthesis (2007, background): “In Form II enzyme from vestimentarian tubeworm symbionts, Robinson et al. 2003 found ε to be 19.5‰ at 30 °C and pH ~7.”
Are spatial variations in the diets of hydrothermal fauna linked to local environmental conditions (2009, background): “…of vent fluids are hypothesized to influence δ13C and δ15N isotope signatures (Trask and Van Dover 1999, Gebruk et al. 2000, Colaço et al. 2002b, Robinson et al. 2003, Limen and Juniper 2006) but despite known high spatial variability of environmental conditions at vents (Sarrazin et al.…”