Oceanologia No. 55 (1) / 13
Contents
Obituary
Acknowledgements
Papers
-
Relationships between inherent optical properties in the Baltic Sea for application to the underwater imaging problem:
Iosif Levin, Mirosław Darecki, Sławomir Sagan, Tamara Radomyslskaya
-
Validation of SeaWiFS and MODIS Aqua/Terra aerosol products in coastal regions of European marginal seas:Frédéric Mélin, Giuseppe Zibordi, Thomas Carlund, Brent N. Holben, Sabina Stefan
-
Influence of the parametrization of water optical properties on the modelled sea surface temperature in the Baltic Sea: Małgorzata Stramska, Agata Zuzewicz
-
Comparison of primary productivity estimates in the Baltic Sea based on the DESAMBEM algorithm with estimates based on other similar algorithms:
Małgorzata Stramska, Agata Zuzewicz
-
Surface wave generation due to glacier calving: Stanisław R. Massel, Anna Przyborska
-
Modellingflow in the porous bottom of the Barents Sea shelf: Stanisław R. Massel
-
Influence of landfast ice on the hydrography and circulation of the Baltic Sea coastal zone:
Ioanna Merkouriadi, Matti Leppäranta
-
Habitat modelling limitations - Puck Bay, BalticSea - a case study:
Jan Marcin Węsławski, Lucyna Kryla-Straszewska, Joanna Piwowarczyk, Jacek Urbański, Jan Warzocha, Lech Kotwicki, Maria Włodarska-Kowalczuk, Józef Wiktor
-
Spatio-temporal variation of microphytoplankton in the upwelling system of the south-eastern Arabian Sea during the summer monsoon of 2009:
Lathika Cicily Thomas, K. B. Padmakumar, B. R. Smitha, C. R. Asha Devi, S. Bijoy Nandan, V. N. Sanjeevan
-
Summer mesozooplankton community of Moller Bay (Novaya Zemlya Archipelago, Barents Sea):
Vladimr G. Dvoretsky,Alexander G. Dvoretsky
-
Seasonal fluxes of phosphate across the sediment-water interface in Edku Lagoon, Egypt:
Mona Kh. Khalil,Ahmed E. Rifaat
-
First records of polychaetes new to Egyptian Mediterranean waters:
Mohamed Moussa Dorgham, Rasha Hamdy, Hoda Hassan El-Rashidy, Manal Mohamed Atta
Communications
Papers
Relationships between inherent optical properties in the Baltic Sea for application to the underwater imaging problem
Oceanologia 2013, 55(1), 11-26
http://dx.doi.org/10.5697/oc.55-1.011
Iosif Levin2, Mirosław Darecki1, Sławomir Sagan1, Tamara Radomyslskaya2
1Institute of Oceanology, Polish Academy of Sciences,
Powstańców Warszawy 55, Sopot 81-712, Poland;
e-mail: darecki@iopan.gda.pl
2St. Petersburg Branch of the P.P. Shirshov Institute of Oceanology of the Russian Academy of Sciences (IO RAS),
1 Linia 30, 199053, St. Petersburg, Russia;
e-mail: ocopt@yandex.ru
keywords:
Baltic Sea, underwater visibility, light attenuation, optical properties
Received 2 August 2012, revised 18 September 2012, accepted 19 November 2012.
This work was supported by the Russian Foundation for Basic Research project No. 10-05-00311. Partial support for this study was also provided by the Satellite Monitoring of the Baltic Sea Environment - SatBaltyk project,
funded by the European Union through European Regional Development Fund contract No. POIG 01.01.02-22-011/09 and statutory research funds from the Institute of Oceanology PAS, Sopot.
Abstract
Statistical relationships between coefficients of light attenuation, scattering and
backscattering at wavelength 550 nm derived from series of optical measurements
performed in Baltic Sea waters are presented. The relationships were derived
primarily to support data analysis from underwater imaging systems. Comparison
of these relations with analogous empirical data from the Atlantic and Pacific
Oceans shows that the two sets of relationships are similar, despite the different
water types and the various experimental procedures and instrumentation applied.
The apparently universal character of the relationships enables an approximate
calculation of other optical properties and subsequently of the contrast, signal/noise
ratio, visibility range and spatial resolution of underwater imaging systems based
on attenuation coefficients at wavelength 550 nm only.
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Validation of SeaWiFS and MODIS Aqua/Terra aerosol products in coastal regions of European marginal seas
Oceanologia 2013, 55(1), 27-51
http://dx.doi.org/10.5697/oc.55-1.027
Frédéric Mélin1, Giuseppe Zibordi1, Thomas Carlund2, Brent N. Holben3, Sabina Stefan4
1European Commission - Joint Research Centre, Institute for Environment and Sustainability
TP272, Ispra, 21027, Italy
2Swedish Meteorological and Hydrological Institute,
SE-601 76, Norrköping, Sweden
3Goddard Space Flight Center, National Aeronautics and Space Administration,
Greenbelt, Maryland 20771, USA
4University of Bucharest, Faculty of Physics,
077125 Magurele, P.O. BOX MG-11, Bucharest, Romania
keywords:
aerosols, ocean colour, AERONET, validation, European seas
Received 5 September 2012, revised 26 November 2012, accepted 18 December 2012.
Abstract
The aerosol products associated with the ocean colour missions SeaWiFS and
MODIS (both Aqua and Terra) are assessed with AERONET field measurements
collected in four European marginal seas for which fairly large uncertainties in
ocean colour in-water products have been documented: the northern Adriatic, the
Baltic, Black and North Seas. On average, more than 500 match-ups are found
for each basin and satellite mission, showing an overall consistency of validation
statistics across the three missions. The median absolute relative difference
between satellite and field values of aerosol optical thickness τa
at 443 nm varies from 12% to 15% for the three missions at the northern
Adriatic and Black Sea sites, and from 13% to 26% for the Baltic and North Sea sites.
It is in the interval 16-31% for the near-infrared band. The spectral shape of τais
well reproduced with a median bias of the Ängström exponent varying
between -15% and +14%, which represents a clear improvement with respect
to previous versions of the atmospheric correction scheme. These results show
that the uncertainty associated with τa in the considered coastal
waters of the European marginal seas is comparable to global validation
statistics.
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Influence of the parametrization of water optical properties on the modelled sea surface temperature in the Baltic Sea
Oceanologia 2013, 55(1), 53-76
http://dx.doi.org/10.5697/oc.55-1.053
Małgorzata Stramska1,2,*, Agata Zuzewicz1,2
1Institute of Oceanology, Polish Academy of Sciences,
Powstańców Warszawy 55, Sopot 81-712, Poland;
e-mail: mstramska@iopan.gda.pl
*corresponding author
2Department ofEarth Sciences, Szczecin University,
Mickiewicza 16, Szczecin 70-383, Poland
keywords:
Baltic Sea, sea surface temperature, biological-physical interactions, ocean models
Received 18 July 2012, revised 6 November 2012, accepted 26 November 2012.
This work was supported by the SatBałtyk project funded by the European Union through the European Regional Development Fund
(contract No. POIG.01.01.02-22-011/09 entitled "The Satellite Monitoring of the Baltic Sea Environment").
Abstract
Treatment of light propagation in the water column requires further
improvements in the biogeochemical models of the Baltic Sea. Regional models of the Baltic
Sea usually assume a simple exponential vertical distribution of the total
downward irradiance in the visible spectral range (PAR, photosynthetically
available radiation). This is in spite of the fact that modelling studies
for open ocean regions have stressed the importance of more detailed optical
parameterization for the quality prediction of sea surface temperature and
thermal structure of surface waters. In recent years extensive regional
in situ bio-optical data sets have become available for the Baltic Sea,
which can be used to develop a better understanding of the feedbacks
between optics and other processes simulated by the models. In this paper
we compare four optical parameterizations used in numerical ocean models
and their effects on modelled SSTs. This has been achieved using a
one-dimensional ocean model coupled with the bio-optical models. Our results
indicate that the differences between the various modelled SSTs using
three optical parameterization schemes designed specifically for the
Baltic Sea can give differences of up to 4°Cin the modelled SSTs.
This result warrants further research into the subject.
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Comparison of primary productivity estimates in the Baltic Sea based on the DESAMBEM algorithm with estimates based on other similar algorithms
Oceanologia 2013, 55(1), 77-100
http://dx.doi.org/10.5697/oc.55-1.077
Małgorzata Stramska1,2,*, Agata Zuzewicz1,2
1Institute of Oceanology, Polish Academy of Sciences,
Powstańców Warszawy 55, Sopot 81-712, Poland;
e-mail: mstramska@iopan.gda.pl
*corresponding author
2Department ofEarth Sciences, Szczecin University,
Mickiewicza 16, Szczecin 70-383, Poland
keywords:
ocean colour, satellite remote sensing, primary productivity, Baltic Sea
Received 12 July 2012, revised 26 October 2012, accepted 4 January 2013.
This work was supported through the SatBałtyk project funded by the European Union through the European Regional Development Fund,
(contract No. POIG.01.01.02-22-011/09 entitled "The Satellite Monitoring of the Baltic Sea Environment").
Abstract
The quasi-synoptic view available from satellites has been broadly used
in recent years to observe in near-real time the large-scale
dynamics of marine ecosystems and to estimate primary productivity
in the world ocean. However, the standard global NASA ocean colour
algorithms generally do not produce good results in the Baltic Sea.
In this paper, we compare the ability of seven algorithms to estimate
depth-integrated daily primary production (PP, mg C m-2)
in the Baltic Sea. All the algorithms use surface chlorophyll
concentration, sea surface temperature, photosynthetic available
radiation, latitude, longitude and day of the year as input data.
Algorithm-derived PP is then compared with PP estimates obtained
from 14C uptake measurements. The results indicate that
the best agreement between the modelled and measured PP in the Baltic Sea
is obtained with the DESAMBEM algorithm. This result supports the
notion that a regional approach should be used in the interpretation
of ocean colour satellite data in the Baltic Sea.
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Surface wave generation due to glacier calving
Oceanologia 2013, 55(1), 101-127
http://dx.doi.org/10.5697/oc.55-1.101
Stanisław R. Massel, Anna Przyborska
Institute of Oceanology, Polish Academy of Sciences,
Powstańców Warszawy 55, Sopot 81-712, Poland;
e-mail: smas@iopan.gda.pl
*corresponding author
keywords:
glacier calving, surface waves, pressure impulse, integral transforms
Received 09 September 2012, revised 21 October 2012, accepted 26 November 2012.
The authors are grateful for support from the Arctic and Environment of the Nordic
Seas and the Svalbard-Greenland Area (AWAKE) Grant.
Abstract
Coastal glaciers reach the ocean in a spectacular process called "calving".
Immediately after calving, the impulsive surface waves are generated,
sometimes of large height. These waves are particularly dangerous for vessels
sailing close to the glacier fronts. The paper presents a theoretical model
of surface wave generation due to glacier calving. To explain the wave generation process, four case
studies of ice blocks fallinginto water are discussed: a cylindrical ice block of small thickness impacting on
water, an ice column sliding into water without impact, a large ice block
falling on to water with a pressure impulse, and an ice column becoming
detached from the glacier wall and falling on to the sea surface. These case
studies encompass simplified, selected modes of the glacier calving, which can
be treated in a theoretical way. Example calculations illustrate the predicted
time series of surface elevations for each mode of glacier calving.
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Modellingflow in the porous bottom of the Barents Sea shelf
Oceanologia 2013, 55(1), 129-146
http://dx.doi.org/10.5697/oc.55-1.129
Stanisław R. Massel
Institute of Oceanology, Polish Academy of Sciences,
Powstańców Warszawy 55, Sopot 81-712, Poland;
e-mail: smas@iopan.gda.pl
keywords:
porous media, surface waves, tides, Ekman layer
Received 18 October 2012, revised 21 November 2012, accepted 26 November 2012.
Abstract
In their recent paper, Węsławski et al. (2012)showed that the
Svalbardbankenarea of the Barents Sea is characterized by a high organic
carbon settlement to the permeable sea bed, whichconsists of gravel and
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of water flow can be substantial, even at large water depths.
During stormy weather (wind velocity V=15 m s-1 and wind
fetch X =200 km) as much as 117.2 and 26.1 m3 hour-1 of
water filter through the upper 5 m of the shell pit at water
depths of 30 and 50 m respectively. For a porous layer of
greater thickness, the mean flow discharge is even bigger.
The second possible mechanism of flow penetration in the porous layer
is based on the concept of geostrophic flow andspiral formation within
the Ekman layer. Assuming that the current velocity in the near-bottom
water layer isū = 1 m, the resulting mean discharge
through this layer becomes as large as 0.99 and 0.09 m3 s-1
for downstream and transverse flows respectively.
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Influence of landfast ice on the hydrography and circulation of the Baltic Sea coastal zone
Oceanologia 2013, 55(1), 147-166
http://dx.doi.org/10.5697/oc.55-1.147
Ioanna Merkouriadi, Matti Leppäranta
Department of Physics, University of Helsinki,
P.O. Box 48 (Erik Palménin aukio 1), Fi-00014 Helsinki, Finland;
e-mail: ioanna.merkouriadi@helsinki.fi
e-mail: matti.lepparanta@helsinki.fi
keywords:
Gulf of Finland, coastal sea ice, hydrography, currents
Received 24 October 2012, revised 4 February 2013, accepted 8 February 2013.
Abstract
The influence of landfast ice on hydrography and circulation is examined in
Santala Bay, adjacent to the Hanko Peninsula, Gulf of Finland. Three-dimensional
electromagnetic current meters and conductivity-temperature-depth (CTD) sensors
were deployed in winters 1999-2000 and 2000-2001 during the Finnish-Japanese
"Hanko 9012" experiment. In each winter, data collection started one month before
the initial ice formation and lasted until one month after the ice had melted
completely. Temperature and salinity are compared with long-term data from the
Tvärminne Zoological Station, also located on the Hanko Peninsula. The
water temperature was 2°C less than the long-term average. Ice
formation and melting show up in the salinity evolution of the water body,
which makes salinity a good indicator of ice formation and breakup in Santala
Bay. The circulation under the ice became weaker by almost 1 cm s-1.
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Habitat modelling limitations - Puck Bay, BalticSea - a case study
Oceanologia 2013, 55(1), 167-183
http://dx.doi.org/10.5697/oc.55-1.167
Jan Marcin Węsławski1,*,
Lucyna Kryla-Straszewska2,3,
Joanna Piwowarczyk1,
Jacek Urbański3,4,
Jan Warzocha5,
Lech Kotwicki1,
Maria Włodarska-Kowalczuk1,
Józef Wiktor1
1Institute of Oceanology, Polish Academy of Sciences,
Powstańców Warszawy 55, Sopot 81-712, Poland;
e-mail: weslaw@iopan.gda.pl
*corresponding author
2International Association of Oil and Gas Producers (OGP),
209-215 Blackfriars Road, SE1 8NL, London, United Kingdom
3Centrum GIS WOiG,
Bażyńskiego 4, 80-952 Gdańsk, Poland
4Institute of Oceanography, University of Gdańsk,
al. Marszałka Piłsudskiego 36, 81-378 Gdynia, Poland
5National Marine Fisheries Research Institute,
Kołłątaja 1, 81-332 Gdynia, Poland
keywords:
species distribution, seabed, habitat modelling, spatial and temporal boundaries,ecosystem-based management
Received 18 September 2012, revised 21 January 2013, accepted 24 January 2013.
This study represents a contribution to the project "Advanced Modelling Tool for Scenarios of
the Baltic Sea Ecosystem to Support Decision Making (ECOSUPPORT)", which has received funding
from the EC's Seventh Framework Programme (FP/2007-2013, Grant 217246)
in conjunction with BONUS, the joint Baltic Sea research and development programme, supported by the Polish Ministry of
Science and Higher Education (Grant 06/BONUS/2009). It also contributes to the Habitat
Mapping project ("Ecosystemapproachto marinespatialplanning - Polish Marine Areas and the Natura2000
network", PL 0078),supported by a grant from Iceland, Liechtenstein and Norway through the EEA Financial Mechanism.
Abstract
TheNatura 2000 sites and the Coastal Landscape Park in ashallow marine bay in thesouthern Baltic have been studied in
detail for thedistribution of benthic macroorganisms, species assemblages and seabed habitats. The
relatively small Inner Puck Bay (104.8 km2) isone of themost thoroughly investigated marine areas
in the Baltic: research has been carried out there continuously for over 50 years. Six physical parameters regarded as critically important for the marine benthos (depth, minimal temperature, maximumsalinity, light, wave intensity and sediment type) were summarized on aGIS map showing unified patches of seabed and the near-bottom water conditions.
The occurrence of uniform seabed forms is weakly correlatedwith the distributions of individual species or multi-species assemblages.This is partly explained by the characteristics of thelocal macrofauna, which is
dominated by highly tolerant, eurytopic species with opportunistic strategies.
The history and timing of the assemblage formationalso explains this weak correlation.The distribution of assemblages formed by
long-living, structural species (Zostera marinaand other higher plants) shows the history of recovery following
earlierdisturbances. In the study area, these communities are still in thestage of recovery and recolonization,
and their present distribution does not as yet match the distribution of the physical environmental conditions favourable
to them. Our results show up the limitationsof distribution modelling in coastal waters, where thehistory of anthropogenic disturbances can distort the picture of the present-day environmental control of biota distributions.
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Oceanologia 2013, 55(1), 185-204
http://dx.doi.org/10.5697/oc.55-1.185
Lathika Cicily Thomas1,*,
K. B. Padmakumar1,
B. R. Smitha1,
C. R. Asha Devi1,
S. Bijoy Nandan2,
V. N. Sanjeevan1
1Centre for Marine Living Resources and Ecology, Ministry of Earth Sciences,
Kochi-37, Kerala, India;
e-mail: lathikacicily@gmail.com;
*corresponding author
2Department of Marine Biology, Microbiology & Biochemistry,
School of Marine Sciences, Cochin University of Science and Technology,
Kochi-16, Kerala, India
keywords:
South Eastern Arabian Sea, upwelling, coastal waters, phytoplankton, chlorophyll a, diatoms
Received 14 May 2012, revised 9 November 2012, accepted 15 November 2012.
This investigation was conducted under the Marine Living Resources Programme funded by the Ministry of Earth Sciences,
Government of India, New Delhi.
Abstract
The phytoplankton standing crop was assessed in detail along the South Eastern Arabian Sea (SEAS) during the different phases of coastal upwelling in 2009. During phase 1 intense upwelling was observed along the southern transects
(8°N and 8.5°N). The maximum chlorophyll aconcentration (22.7 mg m-3) was observed
in the coastal waters off Thiruvananthapuram (8.5°N). Further north there was no signature of upwelling, with extensive Trichodesmium erythraeum blooms. Diatoms dominated in these upwelling regions with the
centric diatom Chaetoceros curvisetus being the dominant species along the 8°N transect. Along the 8.5°N transect pennate diatoms like Nitzschia seriata and Pseudo-nitzschia sp. dominated. During
phase 2, upwelling of varying intensity was observed throughout the study area with maximum chlorophyll a concentrations along the 9°N transect (25 mg m-3) with Chaetoceros curvisetus as the dominant
phytoplankton.Along the 8.5°N transect pennate diatoms during phase 1 were replaced by centric diatoms like Chaetoceros sp. The presence of solitary pennate diatoms Amphora sp. and Navicula sp.
were significant in the waters off Kochi.Upwelling was waning during phase 3 and was confined to the coastal waters of the southern transects with the highest chlorophyll aconcentration of 11.2 mg m-3. Along with
diatoms, dinoflagellate cell densities increased in phases 2 and 3. In the northern transects (9°N and 10°N) the proportion of dinoflagellates was comparatively higher and was represented mainly by Protoperidinium spp., Ceratium spp. and Dinophysis spp.
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Seasonal fluxes of phosphate across the sediment-water interface in Edku Lagoon, Egypt
Oceanologia 2013, 55(1), 219-233
http://dx.doi.org/10.5697/oc.55-1.219
Mona Kh. Khalil, Ahmed E. Rifaat
National Institute of Oceanography, and Fisheries (NIOF),
Al Anfushi 21556, Alexandria, Egypt;
e-mail: mona_kh_kh@hotmail.com;
e-mail: aerifaat@yahoo.co.uk
keywords:
phosphorus, geochemical processes, modelling, coastal lagoon, Edku Lagoon
Received 29 March 2012, revised 13 December 2012, accepted 7 January 2013.
Abstract
Edku Lagoon is a shallow, brackish, coastal wetland located in the
north-western part of the Nile Delta. It suffers from a high level of
eutrophication, owing to the heavy load of nutrients, especially phosphorus.
The purpose of this paper was to study the flux rates of organic and inorganic
phosphorus across the sediment water interface in Edku Lagoon. Both the
organic and inorganic phosphorus of surface sediments, pore water and their
concentrations in the water just above the sediments were used to calculate
the flux rates and to derive the geochemical models. These suggest that, at
present, the flux of inorganic and organic phosphorus is from water to
sediments via the sedimentation of inorganic particles and organic matter. The
results show that phosphorus deposition to the sediments exceeds the rate of
inorganic phosphorus release from the sediments to the water column. In a
steady state, the rates of organic phosphorus release more or less match the
rates of deposition. These reflect the imbalance (accumulation) of phosphorus
in the geochemical cycle in the lagoon and its highly eutrophic status.
Efforts to control the eutrophication of Edku Lagoon have focused on reducing the
phosphorus input.
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http://dx.doi.org/10.5697/oc.55-1.235
Mohamed Moussa Dorgham*, Rasha Hamdy, Hoda Hassan El-Rashidy, Manal Mohamed Atta
Department of Oceanography, Faculty of Science, Alexandria University,
Alexandria, 21511, Egypt;
e-mail: mdorgham1947@yahoo.com
*corresponding author
keywords:
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Received 4 September 2012, revised 5 November 2012, accepted 19 November 2012.
Abstract
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Communications
Compensatory growth of the bloom-forming dinoflagellate Prorocentrum donghaiense induced by nitrogen stress
Oceanologia 2013, 55(1), 269-276
http://dx.doi.org/10.5697/oc.55-1.269
Zhuoping Cai1,2, Shunshan Duan2, Honghui Zhu1,*
Guangdong Institute of Microbiology,
Guangdong Provincial Key Laboratory of Microbial Culture Collection and Application,
Guangdong Open Laboratory of Applied Microbiology, State Key Laboratory of Applied Microbiology
(Ministry-Guangdong Province Jointly Breeding Base),
South China, Guangzhou 510070, China;
e-mail: zhuhonghui66@yahoo.com.cn;
*corresponding author
2Institute of Hydrobiology, Jinan University,
Guangzhou 510632, China;
e-mail: zhuopingcai@yahoo.com
keywords:
compensatory growth, Prorocentrum donghaiense, nitrogen
Received 21 November 2012, revised 13 February 2013, accepted 18 February 2013.
This study was supported by the Natural Science Foundation of China-Guangdong
Province Joint Key Project (U1133003), Natural Science Foundation of
China (41176104, 31070103), and Natural Science Foundation of Guangdong
Province Key Project (10251007002000001).
Abstract
Although the phenomenon of compensatory growth has been documented in some
animals and higher plants, little information is available on its manifestation in marine
microalgae. We have conducted the first study on the compensatory growth of the red tide causative dinoflagellate Prorocentrum
donghaiense after its recovery from different nitrogen concentrations.
The results showed that NaNO3 concentrations of 0 and 7.5 mg l-1 significantly reduced the
growth ofP. donghaiense, as compared to 37.5 and 75 mg l-1. When the microalgal cells were returned
to 75 mg l-1, they exhibited subsequent compensatory growth. The most significant compensatory growth was found in
those cells previously experiencing 0 mg dm3, followed by 7.5 mg dm3, indicating that
compensatory growth depended on the extent of nitrogen stress they had been subjected to. Our results suggest that
compensatory growth can be induced in the marine microalga P. donghaiense after its recovery from nitrogen fluctuation,
and that this should be taken into consideration in the prevalence of P. donghaiense blooms in coastal waters.
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