457
Fluorescent Dissolved Organic Matter in Natural Waters
(continued)
Table 2 (contniued)
Fluorescent components
Components identified and sources
Fluorescence properties
References
Peak C-region
Peak A-region Peak T-region Peak T
UV -region
Peak C
Peak M
p
Peak M
Peak W
Major
Minor
EX/Em (nm)
Autochthonous fulvic acid
(C-like)?, fresh and Florida
Bay waters, Florida coastal
Everglades
Component 1,
autochthonous
Peak′
–
–
–
Peak′
–
–
–
Chen et al. (2010)
Autochthonous fulvic acid
(C-like), Lake Taihu
Component 1,
phytoplankton
365/453
–
–
–
270/453
–
–
–
Zhang et al. (2009a)
Autochthonous fulvic acid
(C-like)?, Sepetiba Bay,
Brazil
Component 1,
phytoplankton
350/400–450 –
–
–
275/400–450 –
–
–
Luciani et al. (2008)
Autochthonous fulvic acid
(C-like), Sea ice, Baltic Sea
coastal regions RU
Component 1
Peak′
–
–
–
Peak′
–
–
–
Stedmon et al. (2007a)
Autochthonous fulvic acid
(C-like), deep waters of
the Okhotsk Sea and North
Pacific Ocean
Component 1
370/466
–
–
–
<260/466
–
–
–
Yamashita et al.
(2010)
Autochthonous fulvic acid
(C-like)?, Southern Ocean
Component 3
340/420
–
–
–
260/420
–
–
–
Wedborg et al. (2007)
Autochthonous fulvic acid
(C-like), north Pacific and
Atlantic oceans (Kauai
model)
Component 8 (P8) c
,
autochthonous
355/434
–
–
–
260/434
–
–
–
Murphy et al. (2008)
Humic-like, marine waters
Algae or
phytoplankton
330–350/420–
480
–
–
–
250–260/420–
480
–
–
–
Coble (1996), Parlanti
et al. (2000)
Autochthonous fulvic acid
(M-like): biologically produced
Marine humic-like, marine
waters
Algae or phytoplankton
–
–
310–320/
380–420
–
Peak′
–
–
–
Coble (1996), Parlanti
et al. (2000)