P. King et al., ANALYSIS OF TOTAL AND ORGANIC-CARBON AND TOTAL NITROGEN IN SETTLING OCEANIC PARTICLES AND A MARINE SEDIMENT - AN INTERLABORATORY COMPARISON, Marine chemistry, 60(3-4), 1998, pp. 203-216
10 laboratories, using their routine methods, collaborated in a compar
ison of analyses of total carbon, nitrogen and organic carbon in a sin
gle sample of marine sediment and a pooled sample of settling particul
ate material collected by sediment trap. The standard error of the mea
ns from all individual laboratories was +/-3% of the mean for all tota
l carbon results, and for total nitrogen in the marine sediment, but w
as +/-7% of the mean for total nitrogen in the sediment trap material.
Larger errors (+/-8% of the mean) were found for organic carbon resul
ts from both the marine sediment and the sediment trap material, with
a range of results (expressed as a percentage of the untreated dry wei
ght) for the sediment trap sample analyzed here of 5.60-8.03%. When th
is range is compared with that of particulate organic carbon concentra
tion in sediment trap material obtained by different workers at variou
s deep ocean sites (2.4-10.2%) [Wefer, G., 1989. Particle flux in the
ocean: Effects of episodic production, in: W.H. Berger, V.S. Smetacek,
G. Wefer (Eds.), Productivity of the Ocean: Present and Past, John Wi
ley & Sons, pp, 139-154.] it is apparent that a large proportion of th
e observed oceanic variability could be accounted for by difference in
analytical technique. We suggest that the problem stems from the diff
iculty of accurate separation of the organic and inorganic phases and
discuss the inaccuracies involved in the separation. We present eviden
ce that the range of results is partly due to either volatilisation of
organic carbon during acid treatment, or incomplete removal of organi
c matter during thermal treatment. Lf results from different laborator
ies are to be compared, as is presently required for basin scale and g
lobal studies of ocean carbon cycling and budgets, there is clearly a
need for suitable reference materials, rigorous intercalibration and t
echnique development. (C) 1998 Elsevier Science B.V.