Variation of the photosynthetic electron transfer rate and electron requirement for daily net carbon fixation in Ariake Bay, Japan
Fast repetition rate fluorometry (FRRf) provides a potential means to examine marine primary productivity; however, FRRf-based productivity estimations require knowledge of the electron requirement ( K ) for carbon (C) uptake ( K C ) to scale an electron transfer rate (ETR) to the CO 2 uptake rate....
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Published in | Journal of oceanography Vol. 72; no. 5; pp. 761 - 776 |
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Main Authors | , , , , , , |
Format | Journal Article |
Language | English |
Published |
Tokyo
Springer Japan
01.10.2016
Springer Nature B.V |
Subjects | |
Online Access | Get full text |
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Summary: | Fast repetition rate fluorometry (FRRf) provides a potential means to examine marine primary productivity; however, FRRf-based productivity estimations require knowledge of the electron requirement (
K
) for carbon (C) uptake (
K
C
) to scale an electron transfer rate (ETR) to the CO
2
uptake rate. Most previous studies have derived
K
C
from parallel measurements of ETR and CO
2
uptake over relatively short incubations, with few from longer-term daily-integrated periods. Here we determined
K
C
by comparing depth-specific, daily ETRs and CO
2
-uptake rates obtained from 24-h on-deck incubation experiments undertaken on seven cruises in Ariake Bay, Japan, from 2008 to 2010. The purpose of this study was to determine the extent of variability of
K
C
and to what extent this variability could be reconciled with the prevailing environmental conditions and ultimately to develop a method for determining net primary productivity (NPP) based on FRRf measurements. Both daily ETR and
K
C
of the upper layer varied considerably, from 0.5 to 115.7 mmol e
−
mg Chl-
a
−1
day
−1
and 4.1–26.6 mol e
−
(mol C)
−1
, respectively, throughout the entire data set. Multivariate analysis revealed a strong correlation between daily photosynthetically active radiation (PAR) and
K
C
(
r
2
= 0.94). A simple PAR-dependent relationship derived from the data set was used for generating
K
C
, and this relationship was validated by comparing the FRRf-predicted NPP with the
13
C uptake measured in 2007. These new observations demonstrate the potential application of FRRf for estimating regional NPP from ETR. |
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Bibliography: | ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 23 |
ISSN: | 0916-8370 1573-868X |
DOI: | 10.1007/s10872-016-0370-4 |