Phytoplankton and the physical environment in the Helgoland region

The phytoplankton development in the waters around Helgoland can be described as a function of the physical environment (derivates of the temperature). This is a consequence of the fundamental annual cycle regulated by the sun and, respectively, by dependent components. This simple statement can only give good results if the turbulent transport processes in the transition zone are considered. Investigations are impeded by the fact that the multiplication rate of the organisms is almost counterbalanced by losses that take place during the long lasting bloom. This situation is a product of the regional hydrography, whereby small changes in the environment on varied time scales influence the development of the population fundamentally. This becomes particularly clear when the numerical results of the exponential growth are examined. The dynamics of this complicated process can be seen best in the great annual differences of the phytoplankton maxima.     

Phytoplankton biomass and production during late austral spring (1991) and summer (1993) in the Bransfield Strait

Phytoplankton biomass and productivity were measured during two cruises in the Bransfield Strait in December 1991 (D91) and January/February 1993 (J93). Strong seasonal variability in productivity values was observed due to differences in the physiological response of phytoplankton. However, although the photosynthetic capacity of phytoplankton was markedly lower in D91 [P _m ^B =0.61 ± 0.25 mg C (mg Chla)⁻¹ h⁻¹] than in J93 [P _m ^B =2.18 ± 0.91 mg C (mg Chla)⁻¹ h⁻¹], average water column chlorophyll values in different areas of the strait were approximately similar in D91 (49–78 mg Chla m⁻²) and J93 (22–76 mg Chla m⁻²). The spatial distribution of chlorophyll was patchy and generally associated with the influence of the different water masses that meet together in the Bransfield Strait. No correlation was found between the mixed layer depth and either the integrated chlorophyll or the productivity. Our results suggest that major phytoplankton blooms in the Bransfield Strait are advected from the nearby Gerlache Strait or Bellingshausen Sea following the main eastward surface currents. Accepted: 5 July 1998     

Phytoplankton in the physical environment: beyond nutrients, at the end, there is some light

This article summarizes the outcomes of the 15th Workshop of the International Association for Phytoplankton Taxonomy and Ecology. Four major issues dealing with the role of physical factors in phytoplankton ecology were addressed in the articles of this special volume: global change and its likely impacts on phytoplankton, the role of physical factors in the autecology of particular species, impacts on the inocula for the following years, and the role of light in shaping phytoplankton dynamics. Case studies from different types of aquatic environments (rivers, deep and shallow lakes, floodplain lakes, wetlands, oxbows, and even the deep ocean) and from diverse geographical locations (not only from the Mediterranean and temperate regions, but also from subtropical and tropical ones) have shown that physical forcing exerts a variety of selective pressures with impacts ranging from molding shape and size of organisms to modifying, through cascade effects, the structure of whole ecosystems.     

Phytoplankton biomass and primary production in the marginal ice zone of the northwestern Weddell Sea during austral summer

During the austral summer of 1995, distributions of phytoplankton biomass (as chlorophyll a), primary production, and nutrient concentrations along two north-south transects in the marginal ice zone of the northwestern Weddell Sea were examined as part of the 8th Korean Antarctic Research Program. An extensive phytoplankton bloom, ranging from 1.6 to 11.2 mg m⁻³ in surface chlorophyll a concentration, was encountered along the eastern transect and extended ca. 180 km north of the ice edge. The spatial extent of the bloom was closely related to the density field induced by the input of meltwater from the retreating sea ice. However, the extent (ca. 200 km) of the phytoplankton bloom along the western transect exceeded the meltwater-influenced zone (ca. 18 km). The extensive bloom along the western transect was more closely related to local hydrography than to the proximity of the ice edge and the resulting meltwater-induced stability of the upper water column. In addition, the marginal ice zone on the western transect was characterized by a deep, high phytoplankton biomass (up to 8 mg Chl a m⁻³) extending to 100-m depth, and the decreased nutrient concentration, which was probably caused by passive sinking from the upper euphotic zone and in situ growth. Despite the low bloom intensity relative to the marginal ice zone in both of the transects, mean primary productivity (2.6 g C m⁻² day⁻¹) in shelf waters corresponding to the northern side of the western transect was as high as in the marginal ice zone (2.1 g C m⁻² day⁻¹), and was 4.8 times greater than that in open waters, suggesting that shelf waters are as highly productive as the marginal ice zone. A comparison between the historical productivity data and our data also shows that the most productive regions in the Southern Ocean are shelf waters and the marginal ice zone, with emerging evidence of frontal regions as another major productive site. Accepted: 27 September 1998     

Phytoplankton production,biomass and community structure following a summer nutrient pulse in Chesapeake Bay

Unusually high concentrations of NH₄⁺ (up to 10 μM) were observed in the surface waters of polyhaline Chesapeake Bay during July 2000, supporting elevated rates of simulated in situ integrated primary production (4.6 g C m⁻² day⁻¹) and chlorophyll-a (chl-a) specific integrated primary production (56 mg C mg chl-a⁻¹ day⁻¹). These rates were the highest measured in the polyhaline Bay during a 5-year sampling program. Chl-a and the percent contribution of phytoplankton >20 μm to the total phytoplankton increased after the ammonium pulse. We hypothesize that increased wind-driven mixing and a tilting of the pycnocline caused by northeast winds combined to increase the transport of NH₄⁺ from below the pycnocline to the surface water. Summer wind and chl-a data collected in the southern Bay between 1984 and 2000 revealed that chl-a was significantly higher 2 weeks after northeast winds than in years when no northeast wind occurred. Episodic peaks in NH₄⁺ and primary productivity resulting from wind events lasting only a few days are poorly captured by traditional shipboard surveys, but may be detected if sampling is focused on periods when wind forcing favors enhanced NH₄⁺ transport to the surface waters. This process of introduction of NH₄⁺ to the surface water from sediments followed by enhanced primary productivity may help explain some of the phytoplankton blooms that are observed in the polyhaline Bay and other estuaries during summer months.     

Phytoplankton spring bloom in the Tagus coastal waters: hydrological and chemical conditions

Spatial variability of phytoplankton as well as hydrological and chemical conditions in the Tagus coastal waters were studied during the spring of 1994. The highly patchy distribution of phytoplankton and the community structure were related to the specific abiotic conditions prevailing in the area. Two main water masses were distinguished: a tidally mixed one alongshore Lisbon-cape Espichel and a stratified region strongly related to the Tagus plume river. The latter seems to control, to some extent, the spatial phytoplankton variability and the timing and size of the spring bloom. The highest surficial levels of nutrients, specifically PO₄ ^3–=1.00 M, NO₃ ^–=16.0 M and Si(OH)₄=14.6 M, were clearly associated with Tagus river discharges, while the lowest levels were attained offshore in the zone of maximum chlorophyll a concentrations (30 mg m^–3) reflecting the occurrence of high nutrient consumption. Furthermore, the near depletion of PO₄ ^3– indicates P limitation for phytoplankton growth. The diatom Detonula pumila (0.1×10⁶ cells l^–1) was the dominant species of phytoplankton communities in the mixed zone, alongshore Lisbon-cape Espichel, whereas, the small diatom Thalassiosira sp. (3×10⁶ cells l^–1) was blooming offshore, associated with the stratified region.     

Phytoplankton spring blooms in the southern Baltic Sea--spatio-temporal development and long-term trends

The seasonal and long-term development of the phytoplanktonspring bloom in different regions of the southern Baltic Seawas investigated on the basis of monitoring data. The developmentof a spring bloom starts when the upper mixed layer becomesshallower than the euphotic zone, as proved also by a mesocosmexperiment. This already happens in March in Mecklenburg Bightand the western part of the Arkona Sea, leading to a diatombloom, but only in April in the Bornholm Sea, increasingly givingrise to a dinoflagellate bloom. The new production of the springphytoplankton may be calculated from the decrease in nutrientsduring spring. In comparison with the Redfield ratio, phosphorusis taken up in excess (N:P = 9.2–10.2). The consumptionof silicate in spring has been reduced in the southern Balticproper since 1989, pointing to a decline in diatoms. The increasein chlorophyll a in the Bornholm and the southern Gotland Seasis related to eutrophication, whereas the decrease in diatomsin favour of the dinoflagellates is related to mild winters.The lack of deep-reaching circulation after mild winters maybe one reason for the suppression of the non-motile diatoms.     

Phytoplankton community structure during the record Arctic ice-melting of summer 2007

In the summer of 2007, the Arctic Ocean experienced the largest loss of ice cover yet observed. We examined the phytoplankton community composition at several stations in the NE Arctic Sector during the ATOS-Arctic cruise in July 2007, specifically in the Fram Strait and along the permanent ice edge up to 81°N. The prymnesiophyte Phaeocystis pouchetti, present exclusively in its colonial form, dominated the whole phytoplankton community, representing 82.1 ± 3.1% (mean ± SE) of the phytoplankton biovolume in the region. Diatoms, small flagellates and dinoflagellates, expected to dominate the ice-melt waters in this sector of the Arctic Ocean, were practically insignificant, representing 7.3 ± 2.4%, 6.8 ± 1.4% and 4.4 ± 1.2% of phytoplankton biovolume, respectively. The fraction of the phytoplankton biomass that comprised diatoms increased with increasing water temperature and salinity, and was, therefore, negatively associated with the increased load of ice-melt waters. In contrast, the fraction of the biomass that comprised P. pouchetii was not as clearly related to temperature and had a weak tendency to decrease with increasing temperature. This pattern was likely the result of different populations stress, as the percentage of living cells of P. pouchetii increased with increasing salinity and temperature. The exceptional dominance of the colonial form of P. pouchetii during the massive ice losses of summer 2007 provides indication of major changes in phytoplankton community structure and carbon flow with climate change in the Arctic Ocean.     

Phytoplankton community structure and environment in the Kenyan waters of Lake Victoria

• 1 Phytoplankton species composition, numerical abundance, spatial distribution and total biomass measured as chlorophyll a concentration were studied in relation to environmental factors in September 1994 (dry season) and March 1995 (rainy season), respectively, in the Kenyan waters of Lake Victoria; 103 species were recorded.
• 2 Blue‐green algae (Cyanophyceae) were most diverse, followed by diatoms (Bacillariophyceae), green algae (Chlorophyceae) and dinoflagellates (Dinophyceae).
• 3 Twinspan separated the phytoplankton communities in the Nyanza Gulf and those in the open lake during both seasons. During the dry season, the Nyanza Gulf was strongly dominated by blue‐greens, while diatoms dominated in the open lake. During the rainy season, blue‐greens remained dominant in the Nyanza Gulf although the number of species found was lower than during the dry season; in the open lake, blue‐greens replaced diatoms as the dominant group and there were more species than in the dry season.
• 4 Canonical correspondence analysis indicated that the phytoplankton species distribution was significantly correlated with turbidity during the dry season and with SiO₂ during the rainy season. Chlorophyll a concentrations ranging from 2.0 to 71.5 mg m^‐3 in the dry season and 2.0–17.2 mg m^‐3 in the rainy season confirm earlier reports of increasing phytoplankton biomass in Lake Victoria since the 1960s.

     

Phytoplankton in the Marginal Ice Zone of the Greenland Sea during summer, 1984

Summary Phytoplankton biomass and species composition were studied in transects through the ice edge region of the Greeland Sea from 19 July to 8 August 1984. Biomass was estimated by vertical in situ chlorophyll fluorescence and pigment extraction of discrete samples. Preserved material was used for identification of phytoplankton species and calculation of their relative abundances. The results suggest that the various geographical regions of the Greenland Sea differ considerably in their phytoplankton development. Autotrophic biomass and species composition were closely associated with the extent of the annual and seasonal ice cover, hydrographic conditions, nutrient availability and the water masses typical of the different domains. In the NE Greenland polynya a deep mixed layer inhibited the development of a phytoplankton bloom, whereas greatest biomass concentrations were associated with a receding ice edge on the E Greenland Shelf. In the Fram Strait, the position of the relatively stationary ice edge is controlled by frontal dynamics, currents and wind. Due to rapidly changing physical and chemical conditions, phytoplankton biomass showed great variability between stations. High chlorophyll a concentrations may develop locally where melting ice causes stratification or can result from passive accumulation in eddies. In July/August 84 the Fram Strait area was dominated by a typical summer population of flagellates and large diatom species.Contribution 6 of the Alfred-Wegener-Institute for Polar and Marine Research     

Arctic spring: hormone-behavior interactions in a severe environment

Arctic breeding birds arrive on their nesting grounds in spring when weather conditions may still be extreme (low temperature, snow). The brief Arctic summer requires that they begin breeding as early as possible to take advantage of the ephemeral abundance of food to feed young. Failure to adjust to the local phenology results in drastically reduced reproductive success. Hormone-behavior adaptations may have evolved that maximize survival and reproductive success in the Arctic. It has been shown that the interrelationship of testosterone and territorial aggression, as birds arrive on the Arctic breeding grounds, varies according to species and locality. In some, territoriality is extremely brief following which birds become apparently refractory to the effects of testosterone. Others are territorial throughout the breeding season, but the dependence of these behaviors upon activation by testosterone is lost. Extensive data also indicate that Arctic birds modulate the adrenocortical response to acute stress. Secretion of corticosterone in response to a standardized capture stress protocol, used to mimic acute stress as a function of local environmental conditions, varies with the stage in the breeding cycle. Arctic breeding birds modulate the sensitivity of the adrenocortical response to acute stress at both the population and individual levels. These modulations are thought to be adaptations to allow the onset of territorial behavior and breeding in the face of potentially stressful conditions. Behavioral and physiological responses to corticosterone treatment are also diminished. A combination of these two hormone-behavior interrelationships can form important components of the proximate mechanisms by which birds, and other vertebrates, breed successfully in a severe and often capricious environment.     

Phytoplankton structure in the White Sea after summer bloom: Spatial variability in relation to hydrophysical conditions

The species composition and phytoplankton biomass, concentrations of chlorophyll “a” (Chl) and nutrients, concurrent hydrophysical conditions were studied in the south part of the White Sea in July 10–15, 2012 during chlorophyll “a” decrease after summer peak. The water column stability varied, the concentration of dissolved silicon in upper mixed layer was closed to the range favorable for diatoms with exception of areas of intensive tide mixing and areas influenced by waters of Severnaya Dvina River. In surface layer the dinoflagellates dominated excepting of areas with intensive tide mixing where diatoms prevailed. Diatoms provided major contribution to biomass in different stations above, in and under pycnocline and in deep waters out of photic zone. Structural analysis has revealed three phytoplankton communities that corresponded to different depths: communities of photic zone, intermediate and deep layers. Extension of layers inhabited by different communities depended on water column stability and on genesis of water masses. Integrated values of phytoplankton biomass and Chl varied from 250 to 1188 mg С/m², and from 22 to 51 mg/m², correspondently.     

Ultrastructure of the parathyroid gland of the japanese lizard in the spring and summer season

The ultrastructure of the parathyroid glands of adult Japanese lizards (Takydromus tachydromoides) in the spring and summer season was examined. The parenchyma of the gland consists of chief cells arranged in cords or solid masses. Many chief cells contain numerous free ribosomes and mitochondria, well-developed Golgi complexes, a few lysosome-like bodies, some multivesicular bodies and relatively numerous lipid droplets. The endoplasmic reticulum is mainly smooth-surfaced. Cisternae of the rough endoplasmic reticulum are distributed randomly in the cytoplasm. Small coated vesicles of 700-800 Å in diameter are found occasionally in the cytoplasm, especially in the Golgi region. The chief cells contain occasional secretory granules of 150-300 nm in diameter that are distributed randomly in the cytoplasm and lie close to the plasma membrane. Electron dense material similar to the contents of the secretory granules is observed in the enlarged intercellular space. These findings suggest that the secretory granules may be discharged into the intercellular space by an eruptocrine type of secretion. Coated vesicles (invaginations) connected to the plasma membrane and smooth vesicles arranged in a row near the plasma membrane are observed. It is suggested that such coated vesicles may take up extracellular proteins. The accumulation of microfilaments is sometimes recognized. Morphological evidence of synthetic and secretory activities in the chief cells suggests active parathyroid function in the Japanese lizard during the spring and summer season.     

Phytoplankton blooms in a fluctuating environment: the roles of plankton response time scales and grazing

Our new view of planktonic ecosystems states that the picoplanktoncan outcompete the netplankton for nutrients, but are held toa relatively constant biomass because of the short responsetime scales of their protist grazers. The long response timeof the mesozooplankton grazing the netphytoplankton allows theselarger phytoplankton to respond to environmental fluctuationswith large changes in biomass. There is some ambiguity in theliterature, however, over the relative importance of ‘responsetime scales’ versus grazing in controlling the phytoplanktonbiomass. To address this issue, a simple model including explicitresponse time scales and grazing was formulated. The model wasused to explore the influence of these two dynamics in controllingthe response of phytoplankton to sudden changes in the carryingcapacity of the environment. It was applied to the IronEx IIdata to explore the implications of the two types of control.The model supports the hypothesis that the short response timescale of the protists limits the picoplankton biomass. However,it also shows that the zooplankton grazing rate (here representedby a clearance rate a) has a much stronger effect in determiningthe phytoplankton biomass than the response time scale.     

Marine mammal and seabird summer distribution and abundance in the fjords of northeast Cumberland Sound of Baffin Island, Nunavut, Canada

Critical baseline population knowledge is required to properly assess the status of marine mammal and bird populations in the Canadian Arctic and the effects of climate trends on them. To address this need for one significant Arctic region, a boat-based marine mammal and seabird transect survey was conducted in Cumberland Sound fjords during summer 2008. During 173 km effort (20 h), 959 birds were recorded representing at least nine species which were dominated by Common Eiders (Somateria mollissima borealis), Iceland or Glaucous Gulls (Larus glaucoides or Larus hyperboreus), and Black Guillemots (Cepphus grylle), in addition to less common birds including Red-throated and Common Loons (Gavia stellata and Gavia immer), Northern Fulmars (Fulmarus glacialis), and Great or Lesser Black-backed Gulls (Larus marinus or Larus fuscus). Of these, 480 birds were observed on the water in one event consisting of eiders and gulls which may have biased encounter rates. Of 101 marine mammal sightings, four species were represented: 73 harp seals (Pagophilus groenlandicus), 13 beluga whales (Delphinapterus leucas), nine bowhead whales (Balaena mysticetus), five ringed seals (Pusa hispida), and one unidentified pinniped. A pod of four killer whales (Orcinus orca) was observed off-effort in Pangnirtung Fjord during the survey period. This pilot study provided the first estimates of relative abundance for marine mammals and seabirds in the study area to aid in developing future surveys.     

Phytoplankton composition in the Weddell-Scotia Confluence area during austral spring in relation to hydrography

During the EPOS leg 2 cruise of the RV Polarstern, carried out in late austral spring of 1988–1989, the composition of phytoplankton in relation to the distribution of hydrographic parameters was studied in four successive transects carried out along 49°W and 47°W, across the Weddell-Scotia Confluence (WSC) and the marginal ice zone (which overlapped in part). In all transects, a maximum of phytoplankton biomass was found in the WSC, in surface waters stabilized by ice melting. Different phytoplankton assemblages could be distinguished. North of the Scotia Front (the northern limit of the WSC) diatoms with Chaetoceros neglectus, Nitzschia spp. and (Thalassiosira gravida) dominated the phytoplankton community. This assemblage appeared to have seeded a biomass maximum which occupied, during the first transect, an area of the WSC, south of the Scotia Front. The southernmost stations of the first transect and all the stations to the south of the Scotia Front in the other transects were populated by a flagellate assemblage (with a cryptomonad, Pyramimonas spp. and Phaeocystis sp.) and an assemblage of diatoms (Corethron criophilum and Tropidoneis vanheurkii among others) associated to the presence of ice. During the last three transects, the flagellate assemblage formed a bloom in the low salinity surface layers of the WSC zone. The bulk of the biomass maximum was formed by the cryptomonad which reached concentrations up to 4×10⁶ cells l^–1 towards the end of the cruise. Multivariate analysis is used to summarize phytoplankton composition variation. The relationships between the distribution of the different assemblages and the hydrographic conditions indicate that the change of dominance from diatoms to flagellates in the WSC zone was related to the presence of water masses from different origin.Data presented here were collected during the European Polarstern Study (EPOS) sponsored by the European Science Foundation     

Phytoplankton and bacterioplankton production in a reed-covered water body

Between 1996 and 1998 phytoplanktonic primary production and bacterioplankton production were measured monthly at five sampling stations in the lower Kis-Balaton reservoir. The open water area of the reservoir was rich in phytoplankton and had hypertrophic characteristics, but inside the reed stand (80% of the surface area) phytoplankton biomass and production were substantially (30–50 times) lower. The algal removal efficiency of the lower Kis-Balaton reservoir was 96%. The reservoir had a considerably smaller effect on bacterioplankton removal than on the phytoplankton. The decrease of biomass and production of bacterioplankton in the through-flowing water was approximately 60%. Inside the reed stand the biomass and the production of planktonic bacteria exceeded that of the phytoplankton by several times, suggesting that the release of biodegradable dissolved organic (humic) substances from macrophytes stimulated the metabolism of bacterioplankton. The significant reduction of phytoplankton inside the dense reed stand was primarily the result of the shading effect of the reeds. In the open water area a shading experiment demonstrated that a 1-week residence period for planktonic algae in the reed-covered area was sufficient for their complete elimination. The decomposition of planktonic algae, reed material and the lack of primary production inside the reed stand created oxygen-deficient and phosphorus-rich conditions during the vegetative period. These results suggest that reed-covered water bodies can effectively retain suspended solids and planktonic algae, but because of decomposition processes they cannot retain biologically-available phosphorus.     

Interinsular variations in the spring and summer diet of the Raven Corvus corax in the Canary Islands

This paper presents the first data on the diet of the Raven Corvus corax in the Canary Islands, based on analysis of 2315 pellets collected from all of the islands and islets in the archipelago. The Ravens on three groups of island showed differences in diet, but in all cases the diet was clearly omnivorous, both in its qualitative and quantitative composition. It is evident that a broadening of the Raven's trophic niche has occurred in comparison with those living in continental areas. While the diet has a strong plant component on the wetter islands (frequency of occurrence > 87%), an appreciable animal component in the diet (principally vertebrates) is more frequent on the drier islands of the archipelago (frequency of occurrence > 96%). The composition of the plant component of the diet varied markedly from one island to another. Remains of refuse are more commonly found in the Raven's diet on the central and western islands. We concluded that while the animal diet is essential from the bioenergetic point of view, the vegetation diet is only a complementary food source. The Raven plays an important role in seed dispersal among the different habitats within each island.