DISTRIBUTION OF ALGAL CHLOROPHYLL AND CAROTENOID-PIGMENTS IN A STRATIFIED ESTUARY - THE KRKA RIVER, ADRIATIC SEA

被引:44
作者
DENANT, V
SALIOT, A
MANTOURA, RFC
机构
[1] UNIV PARIS 06,PHYS & CHIM MARINES LAB,CNRS,UA 353,TOUR 24-25,4 PL JUSSIEU,F-75252 PARIS 05,FRANCE
[2] PLYMOUTH MARINE LAB,PLYMOUTH PL1 3DH,ENGLAND
关键词
D O I
10.1016/0304-4203(91)90044-W
中图分类号
O6 [化学];
学科分类号
0703 ;
摘要
The detailed distribution of algal chlorophyll and carotenoid pigments was determined around the halocline (freshwater-seawater interface) in the Krka Estuary on the east coast of the Adriatic Sea, in May 1988. After collection of water along the estuary, particulate matter was extracted and analyzed for pigments by high-performance liquid chromotography coupled with absorbance and fluorescence detection. Bottom marine waters were characterized by lower chlorophyll a (chl a) concentration than encountered in surface waters, decreasing downstream from 0.50-mu-g l-1 to 0.16-mu-g l-1 at the marine end-member. The highest concentrations of chl a (up to 26.34-mu-g l-1) were found in the interfacial layer, an particularly at one station located off the city of Sibenik, where high inputs of nutrients supported the accumulation of living algae at the halocline. Fucoxanthin was the most abundant carotenoid, which indicates a euryhaline dominance of diatoms in the estuary, whereas the dinoflagellate-derived carotenoid peridinin was confined to the interfacial and bottom saline waters of the inner estuary. High concentrations of alloxanthin and chl b were found in the interfacial layer, which also suggests an accumulation of Cryptophyceae and green algae in the inner estuary. Phaeophorbides showed higher concentrations in bottom waters than in surface waters, whereas the highest concentrations occurred in the interfacial layer. These high levels could reflect a density trapping of dead cells in an early degradation state, as suggested by the importance of allomerized chl a and chlorophyllide a vs. total chl a, or of faecal pellets originating from zooplankton grazing in the interfacial layer.
引用
收藏
页码:285 / 297
页数:13
相关论文
共 39 条
[31]   ESTUARINE TRANSFORMATION OF ORGANIC-MATTER - SINGLE COALESCENCE EVENTS OF ESTUARINE SURFACE-ACTIVE PARTICLES [J].
SVETLICIC, V ;
ZUTIC, V ;
TOMAIC, J .
MARINE CHEMISTRY, 1991, 32 (2-4) :253-267
[32]  
TANGEN K, 1981, Journal of Plankton Research, V3, P389, DOI 10.1093/plankt/3.3.389
[33]   THE RELATIVE ABUNDANCE OF PHEOPHORBIDE-A AND PHEOPHYTIN-A IN TEMPERATURE MARINE WATERS [J].
VERNET, M ;
LORENZEN, CJ .
LIMNOLOGY AND OCEANOGRAPHY, 1987, 32 (02) :352-358
[34]   VERTICAL-DISTRIBUTION OF PHYTOPLANKTON IN A STRATIFIED ESTUARY [J].
VILICIC, D ;
LEGOVIC, T ;
ZUTIC, V .
AQUATIC SCIENCES, 1989, 51 (01) :31-46
[35]   CHLOROPHYLL BUDGETS - ZOOPLANKTON GRAZING AND PHYTOPLANKTON GROWTH IN A TEMPERATE FJORD AND THE CENTRAL PACIFIC GYRES [J].
WELSCHMEYER, NA ;
LORENZEN, CJ .
LIMNOLOGY AND OCEANOGRAPHY, 1985, 30 (01) :1-21
[36]  
WOLLAST R, 1983, MAJOR BIOGEOCHEMICAL, P285
[37]   FUCOXANTHIN PIGMENT MARKERS OF MARINE-PHYTOPLANKTON ANALYZED BY HPLC AND HPTLC [J].
WRIGHT, SW ;
JEFFREY, SW .
MARINE ECOLOGY PROGRESS SERIES, 1987, 38 (03) :259-266
[38]   A FILM OF ORGANIC-MATTER AT THE FRESH-WATER SEA-WATER INTERFACE OF AN ESTUARY [J].
ZUTIC, V ;
LEGOVIC, T .
NATURE, 1987, 328 (6131) :612-614
[39]  
[No title captured]