Over the years The Institute of Marine Research, has been developed to become the leading body fo... more Over the years The Institute of Marine Research, has been developed to become the leading body for monitoring and exploration of marine ecosystems, development of the aquaculture industry, and science based advices on harvesting of living marine resources in Norway. The institute developed with a steadily growing classical hierarchical organization with departments according to scientific disciplines or ecosystem categories. During
Proceedings of the National Academy of Sciences, 2012
Climate warming can trigger abrupt ecosystem changes in the Arctic. Despite the considerable inte... more Climate warming can trigger abrupt ecosystem changes in the Arctic. Despite the considerable interest in characterizing and understanding the ecological impact of rapid climate warming in the Arctic, few long time series exist that allow addressing these research goals. During a 30-y period of gradually increasing seawater temperature and decreasing sea ice cover in Svalbard, we document rapid and extensive structural changes in the rocky-bottom communities of two Arctic fjords. The most striking component of the benthic reorganization was an abrupt fivefold increase in macroalgal cover in 1995 in Kongsfjord and an eightfold increase in 2000 in Smeerenburgfjord. Simultaneous changes in the abundance of benthic invertebrates suggest that the macroalgae played a key structuring role in these communities. The abrupt, substantial, and persistent nature of the changes observed is indicative of a climate-driven ecological regime shift. The ecological processes thought to drive the observed regime shifts are likely to promote the borealization of these Arctic marine communities in the coming years.
ABSTRACT . The population structure and production of the two autochthonous sympagic amphipods, G... more ABSTRACT . The population structure and production of the two autochthonous sympagic amphipods, Gammarus wilkitzkii and Apherusa glacialis, collected in different categories of sea ice north of Svalbard and in the Fram Strait, were examined. A longevity of 6 years for male G. wilkitzkii and 5–6 years for females was indicated, using a Mixture distribution analysis technique. Growth is best described by the Gompertz growth function. The theoretical maximum body length was estimated to be 53.2 and 45.3 mm, and the corresponding maximum age was estimated to be 7.5 and 6.3 years for males and females, respectively. Juveniles of age classes 0+ and 1+ of G. wilkitzkii were most abundant in first-year ice and were regarded as predominant colonizers of new ice habitats. It is unclear whether juveniles have colonized the ice independently or been released there by females colonizing the new ice. Age classes 2+ and 3+ were numerous in multi-year ice. The growth rate for G. wilkitzkii was low, and lower for females than for males. Highest growth rates were found in an area dominated by old ice. A mean production of 0.0237 g ash-free dry weight year–1 m–2 and a somatic P/B ratio (productivity) of 0.255 year–1 were calculated for the entire set of data. Individuals of age class 4+ were the most productive within the population, while juveniles have little influence on the annual productivity. A. glacialis reached a maximum age of 2 years and age class 0+ was about tenfold more abundant compared to age class 1+, indicating a high mortality rate during the 1st year of life. The population structure seems to be more affected by ice conditions (e.g. floe size) than by the age of the ice.
Polar cod (Boreogadus saida) associated with drifting sea-ice were collected in the western Baren... more Polar cod (Boreogadus saida) associated with drifting sea-ice were collected in the western Barents sea and north of Svalbard with dip-nets while SCUBA-diving in 1986 and 1987. Length-frequency measurements and otolith-readings suggested that the specimens were either one or two years old. The diet of fish from the western Barents sea (first-year ice) consisted mainly of copepods (Calanus finmarchicus, Calanus glacialis) and the hyperiid amphipod Parathemisto libellula. Fish collected north of the Svalbard archipelago (multi-year ice) had a more diverse diet, in which P. libellula and the sympagic amphipod Apherusa glacialis contributed more to the total diet biomass than copepods.
The nature of the substratum is a fundamental factor determining the types of organisms and commu... more The nature of the substratum is a fundamental factor determining the types of organisms and communities found in many terrestrial and benthic habitats. The extent to which this is true in extreme environments was investigated using bryozoan assemblages as model organisms in an Arctic fjord (Kongsfjorden 79°N, 12°E) in summer 2001 using SCUBA. Twenty-seven substrate samples of 0.25 m2 were taken at 10 m depth from the inner glacial basin to the mouth of the fjord. Multivariate analyses revealed four different bryozoan assemblages. The sea floor of the inner basin of Kongsfjorden near the glacial fronts was characterized by low diversity and dominance of the ctenostome species Alcyonidium disciforme Smitt. Highest richness and diversity occurred on rock substratum with mean size >10 cm2, on which the most common species was the pioneer Harmeria scutulata Busk (abundance: 15%). On smaller rocks with mean size 2, the runner-like pioneer species Electra arctica Borg comprised most individuals of the assemblage (98%). Yet another pioneer, Celleporella hyalina Linnaeus, was the most abundant species (49%) on substratum dominated by algae. Thus, in each habitat type, pioneers dominated but different species and to different extents. There was much variation in species composition and abundance within assemblages of heterogeneous habitats, and this study emphasizes the importance of microhabitats and physical conditions. Heterogeneity was evident at scales of
The object of the present investigation was to map the distribution and abundance of sympagic fau... more The object of the present investigation was to map the distribution and abundance of sympagic fauna (= ice fauna) (>350 μm) within the perennial sea ice zone near Svalbard and to study relations between the sympagic fauna and the age and history of its ice substrate. The sampling took place in July/August 1986 and September 1988 using SCUBA-operated sampling gear (suction samplers, plankton nets with especially designed frames for sampling at the sea-ice/seawater interface, and underwater cameras). The amphipods Apherusa glacialis, Onisimus sp., and Gammarus wilkitzkii were the most conspicuous sympagic species both years. Scattered individuals of the amphipods Gammaracanthus loricatus, Weyprechtia penguis and the polychaete Harmathoinae indet. were also recorded. A. glacialis was the most numerous and contributed near 65% of the collected specimens in both years, with a maximum density exceeding 2000 individuals/m2. However, G. wilkitzkii was on average larger, and contributed most to the biomass (1986: 80%; 1988: 77%). The average biomass of sympagic fauna in 1986 and 1988 was estimated to be 4.7 g/m2 and 8.3 g/m2 respectively. Biomass values reported here are ten to hundred times higher than what is found within the seasonal sea ice zone. Autochthonous sympagic species, like A. glacialis, Onisimus sp. and G. wilkitzkii, have a permanent association with ice. The seasonal sea ice zone will thus have to be recolonized every year resulting in lower densities compared to multiyear ice. It is suggested that the speed of the ice leaving the Polar Basin through the Fram Strait is too high for the sympagic fauna to remain its position in the sea ice zone. The result is an annual loss in the order of 7*105 tons of sympagic fauna from the perennial sea ice zone.
The sympagic fauna (= sea ice fauna) of the Barents Sea was investigated on nine (2–5 weeks) crui... more The sympagic fauna (= sea ice fauna) of the Barents Sea was investigated on nine (2–5 weeks) cruises in the period 1983–1988. The amphipods Apherusa glacialis, Onisimus sp. and Gammarus wilkitzkii were the most conspicuous and abundant invertebrate species associated with the ice. Mean biomass-values ranged from 0 to about 2 g/m2, and were less than 0.001 g/m2 in five of the nine cruises. Apherusa glacialis, Onisimus sp. and Gammarus wilkitzkii are regarded as autochthonous sympagic species, and as such dependent upon a permanent ice cover. Allochthonous sympagic species were few and without significant importance. The variations in species abundance and biomass were believed to be closely connected to the age and drift-history of the ice. The density of the sympagic fauna increases as a result of increasing influx of ice into the Barents Sea from the Arctic Ocean. Density of the sympagic fauna were believed to increase with decreasing distance to the multiyear/first-year ice boundary. A. glacialis was found further away from the spreading centers and in higher numbers than the other sympagic species due to its greater motility. No day-night variations in the occurrences of the sympagic fauna were recorded.
The distribution of juvenile benthic invertebrates with respect to their abiotic environment was ... more The distribution of juvenile benthic invertebrates with respect to their abiotic environment was investigated at four locations along a gradient in Kongsfjorden (79°N, 12°E), Spitsbergen, in September 1997. Heavy discharge of inorganic sediments released by the three glaciers was expected to be one of the main structuring factors of benthic communities in the fjord. Juveniles of 76 species/families are identified. Total abundance increases with distance from the fjord head due to the dominance of opportunistic polychaetes, while diversity is highest close to the glacier. Juvenile polychaetes are the most abundant taxon over all stations (92%), followed by bivalves, crustaceans and others. Polychaetes also provide most species (55%) and are the dominant taxon at every station. Their abundance is highly correlated with total organic carbon, indicating that most of them are deposit feeders. Young crustaceans rapidly decrease towards the fjord mouth, probably due to stronger bottom currents. Even though young oligochaetes are exclusively found near the glacier, no species seem to be well adapted to the high sedimentation rate close to the glacier. Juvenile suspension-feeding bivalves seem to be less disturbed by glacial discharge but appear to be more vulnerable to currents on the more exposed sites. The importance of deposit feeders and carnivores increases towards the outer stations. Non-metric multidimensional scaling confirms the distinct gradient in community composition along the fjord. Coupling the biotic data to abiotic factors (depth, bottom-water salinity, bottom-water temperature, sediment grain size and sedimentation rate) using canonical correspondence analysis revealed that hydrographic factors are more responsible for the structuring of the benthic juvenile community at the shallow stations close to the glacier (except the station directly at the glacier). At the outer deeper stations, sediment grain size and related properties may play a more important role.
We describe the summer diets of four seabird species, Kittiwake (Rissa tridactyla), Little Auk (A... more We describe the summer diets of four seabird species, Kittiwake (Rissa tridactyla), Little Auk (Alle alle), Black Guillemot (Cepphus 9rylle) and Brfinnich's Guillemot (rJria lomvia) collected in sea-ice-covered waters near SwLlbard. Birds collected in an area filled with young sea-ice, within the seasonal sea-ice zone, were compared with birds collected from the perennial sea-ice zone dominated by multiyear ice. Pelagic Crustacea and fish dominated tt~e diet of birds feeding in young ice, while sympagic Crustacea and fish were most important in the diet of birds feeding in multiyear ice. Boreogadus saida was the most important fish food item. B. Saida was present in the ice in both areas, while sympagic Crustacea were lacking in the area filled with young ice. Important food items in young k:e were B. saida (Black Guillemots and Kittiwakes), Caianus sp. (Little Auks) and Pandalusborealis (Brfinnich's Guillemot). B. saida (Black Guillemots, Kittiwakes, Brfinnich's Guillemots), Gammarus wilkitzkii (Brfinni~:h's Guillemot, Black Guillemot) and Apherusa glacialis (Little Auk) were most important in multiyear ice.
Svalbard bryozoan communities were investigated along a depth range from the surface to 296 m bet... more Svalbard bryozoan communities were investigated along a depth range from the surface to 296 m between the inner glacial fronts and fjord mouths during 2001 and 2002. The main study area was Kongsfjorden (79°N, 12°E). A total of 137 taxa of bryozoans were identified: 108 to species, 24 to genus, 3 to family, 1 to order and 1 to phylum level. Cluster and multidimensional scaling analyses revealed four distinct assemblages of bryozoans: shallow (0-40 m; 68 taxa), deep (40-296 m; 80 taxa), inner fjordic (three taxa) and an assemblage found on small stones in shallow waters (nine taxa). The inner fjordic assemblage was recorded from the front of tidal glaciers extending about 10 km out into the fjord. In terms of abundance, Celleporella hyalina Linnaeus dominated in shallow areas (18%), Hippothoa arctica Kluge (55%) in deep water, Alcyonidium disciforme Smitt (86%) proximate to glaciers fronts and Electra arctica Borg on small stones (98%).
Arctic ice amphipods are part of the sympagic macrofauna in the Marginal Ice Zone of the northern... more Arctic ice amphipods are part of the sympagic macrofauna in the Marginal Ice Zone of the northern Barents Sea and represent an important link from lower to higher trophic levels in some Arctic marine food chains. The species diversity in this area (1995/1996) consisted of four species: Gammarus wilkitzkii, Apherusa glacialis, Onisimus nanseni and Onisimus glacialis. The larger ice amphipod, G. wilkitzkii, was the most abundant with the highest biomass (>90%), whereas A. glacialis was abundant, but contributed little to the total biomass (<4%). The other two species were found only in small numbers. Both abundance and biomass of ice amphipods decreased along a latitudinal gradient from north to south across the Marginal Ice Zone. Their distribution was also related to the under-ice topography with regard to mesoscale structures (edge,¯at area, dome and ridge). Overall, the abundance and biomass on ridges were much higher in comparison to other mesoscale structures, although edges also showed high abundance, but low biomass. The large G. wilkitzkii was consistently abundant on ridges. The small A. glacialis was predominately associated with edges, but also showed high numbers in dome-shaped areas. The Onisimus species were present in low numbers at all structures, and their biomass contributed <10% on any one structure. The reasons for dierent distribution patterns of the dominant amphipod species under Arctic sea ice are probably related to dierent requirements of the species, especially for food, shelter and physiological conditions.
Zooplankton samples were collected in January 1993 o Dronning Maud Land along a transect from ope... more Zooplankton samples were collected in January 1993 o Dronning Maud Land along a transect from open waters to the marginal ice zone close to the Antarctic ice shelf. Thysanoessa macrura was caught in open waters while Calanoides acutus and Calanus propinquus were mainly sampled between ice¯oes in the marginal ice zone. The``ice-krill'' Euphausia crystallorophias was found over the shelf directly associated with ice¯oes. T. macrura had a lipid content up to 36% of its dry weight with the dominant lipid class, wax ester, accounting for 45±50% of the total lipid. The predominance of 18:1 fatty alcohols is the striking characteristic of the wax esters. Small specimens of E. crystallorophias had lipid levels up to 26% of their dry weight with, unexpectedly, triacylglycerols being the dominant lipid (up to 41% of total lipid). The small levels of wax esters in these animals (3±6% of total lipid) had phytol as a major constituent. Large specimens of E. crystallorophias had up to 34% of their dry weight as lipid, with wax esters (47% of total lipid) dominated by 16:0 and 14:0 fatty alcohols as the major lipid. Calanus propinquus had lipid levels of up to 34% of their dry weight, with triacylglycerols (up to 63% of total lipid) being the dominant lipid. High levels of 22:1 (n-9) fatty acid were present in the triacylglycerols. Calanoides acutus had lipid levels up to 35% of the dry weight with wax esters accounting for up to 83% of total lipid. High levels of (n-3) polyunsaturated fatty acids were recorded with 20:5(n-3), 22:6(n-3) and 18:4(n-3) being the dominant moieties. On the basis of their lipid compositions we deduce that: (1) Calanoides acutus is the strictest herbivore among the four species studied, heavily utilizing the typical spring bloom; (2) T. macrura is essentially omnivorous, probably utilizing the less de®ned bloom situations found in oceanic waters; (3) E. crystallorophias is an omnivore well adapted to utilize both a bloom situation and to feed on ice algae and micro-zooplankton associated with the ice; (4) Calanus propinquus seems to be the most opportunistic feeder of the four species studied, probably grazing heavily on phytoplankton during a bloom and, during the rest of the year, feeding on whatever material is available, including particulates,¯agellates and other ice-associated algae. We conclude that the dierent biochemical pathways generating large oil reserves of dierent compositions, enabling species to utilize dierent ecological niches, are major determinants of biodiversity in polar zooplankton.
Gammarus wilkitzkii, Apherusa glacialis, Onismus nanseni, Onismus glacialis, Boreogadus saida, Pa... more Gammarus wilkitzkii, Apherusa glacialis, Onismus nanseni, Onismus glacialis, Boreogadus saida, Parathemisto libellula and Calanus hyperboreus, collected in late June in the Barents Sea marginal ice zone, contained substantial levels (28±51% of the dry mass) of total lipid, the highest levels (51% and 41% respectively) being in A. glacialis and C. hyperboreus. Neutral lipids were present in greater amounts than polar lipids in all species. Triacylglycerols were major neutral lipids in A. glacialis, G. wilkitzkii and O. nanseni; triacylglycerols and wax esters were present in similar amounts in O. glacialis; higher levels of wax esters than triacylglycerols occurred in P. libellula; wax esters greatly exceeded triacylglycerols in C. hyperboreus, the opposite being true for B. saida. Diatom fatty acid markers were prominent in the triacylglycerols of G. wilkitzkii, O. nanseni, O. glacialis and, particularly, of A. glacialis; 20:1(n-9) and 22:1(n-11) moieties were abundant in wax esters of G. wilkitzkii, O. nanseni, O. glacialis, P. libellula and C. hyperboreus, and in triacylglycerols of B. saida. We deduce that A. glacialis feeds mainly on ice algae and phytodetritus, G. wilkitzkii and the Onismus spp. feed on calanoid copepods as well as ice algae, whereas P. libellula and especially B. saida feed extensively on calanoid copepods.
The distribution of juvenile benthic invertebrates with respect to their abiotic environment was ... more The distribution of juvenile benthic invertebrates with respect to their abiotic environment was investigated at four locations along a gradient in Kongsfjorden (79°N, 12°E), Spitsbergen, in September 1997. Heavy discharge of inorganic sediments released by the three glaciers was expected to be one of the main structuring factors of benthic communities in the fjord. Juveniles of 76 species/families are identified. Total abundance increases with distance from the fjord head due to the dominance of opportunistic polychaetes, while diversity is highest close to the glacier. Juvenile polychaetes are the most abundant taxon over all stations (92%), followed by bivalves, crustaceans and others. Polychaetes also provide most species (55%) and are the dominant taxon at every station. Their abundance is highly correlated with total organic carbon, indicating that most of them are deposit feeders. Young crustaceans rapidly decrease towards the fjord mouth, probably due to stronger bottom currents. Even though young oligochaetes are exclusively found near the glacier, no species seem to be well adapted to the high sedimentation rate close to the glacier. Juvenile suspension-feeding bivalves seem to be less disturbed by glacial discharge but appear to be more vulnerable to currents on the more exposed sites. The importance of deposit feeders and carnivores increases towards the outer stations. Non-metric multidimensional scaling confirms the distinct gradient in community composition along the fjord. Coupling the biotic data to abiotic factors (depth, bottom-water salinity, bottom-water temperature, sediment grain size and sedimentation rate) using canonical correspondence analysis revealed that hydrographic factors are more responsible for the structuring of the benthic juvenile community at the shallow stations close to the glacier (except the station directly at the glacier). At the outer deeper stations, sediment grain size and related properties may play a more important role.
Over the years The Institute of Marine Research, has been developed to become the leading body fo... more Over the years The Institute of Marine Research, has been developed to become the leading body for monitoring and exploration of marine ecosystems, development of the aquaculture industry, and science based advices on harvesting of living marine resources in Norway. The institute developed with a steadily growing classical hierarchical organization with departments according to scientific disciplines or ecosystem categories. During
Proceedings of the National Academy of Sciences, 2012
Climate warming can trigger abrupt ecosystem changes in the Arctic. Despite the considerable inte... more Climate warming can trigger abrupt ecosystem changes in the Arctic. Despite the considerable interest in characterizing and understanding the ecological impact of rapid climate warming in the Arctic, few long time series exist that allow addressing these research goals. During a 30-y period of gradually increasing seawater temperature and decreasing sea ice cover in Svalbard, we document rapid and extensive structural changes in the rocky-bottom communities of two Arctic fjords. The most striking component of the benthic reorganization was an abrupt fivefold increase in macroalgal cover in 1995 in Kongsfjord and an eightfold increase in 2000 in Smeerenburgfjord. Simultaneous changes in the abundance of benthic invertebrates suggest that the macroalgae played a key structuring role in these communities. The abrupt, substantial, and persistent nature of the changes observed is indicative of a climate-driven ecological regime shift. The ecological processes thought to drive the observed regime shifts are likely to promote the borealization of these Arctic marine communities in the coming years.
ABSTRACT . The population structure and production of the two autochthonous sympagic amphipods, G... more ABSTRACT . The population structure and production of the two autochthonous sympagic amphipods, Gammarus wilkitzkii and Apherusa glacialis, collected in different categories of sea ice north of Svalbard and in the Fram Strait, were examined. A longevity of 6 years for male G. wilkitzkii and 5–6 years for females was indicated, using a Mixture distribution analysis technique. Growth is best described by the Gompertz growth function. The theoretical maximum body length was estimated to be 53.2 and 45.3 mm, and the corresponding maximum age was estimated to be 7.5 and 6.3 years for males and females, respectively. Juveniles of age classes 0+ and 1+ of G. wilkitzkii were most abundant in first-year ice and were regarded as predominant colonizers of new ice habitats. It is unclear whether juveniles have colonized the ice independently or been released there by females colonizing the new ice. Age classes 2+ and 3+ were numerous in multi-year ice. The growth rate for G. wilkitzkii was low, and lower for females than for males. Highest growth rates were found in an area dominated by old ice. A mean production of 0.0237 g ash-free dry weight year–1 m–2 and a somatic P/B ratio (productivity) of 0.255 year–1 were calculated for the entire set of data. Individuals of age class 4+ were the most productive within the population, while juveniles have little influence on the annual productivity. A. glacialis reached a maximum age of 2 years and age class 0+ was about tenfold more abundant compared to age class 1+, indicating a high mortality rate during the 1st year of life. The population structure seems to be more affected by ice conditions (e.g. floe size) than by the age of the ice.
Polar cod (Boreogadus saida) associated with drifting sea-ice were collected in the western Baren... more Polar cod (Boreogadus saida) associated with drifting sea-ice were collected in the western Barents sea and north of Svalbard with dip-nets while SCUBA-diving in 1986 and 1987. Length-frequency measurements and otolith-readings suggested that the specimens were either one or two years old. The diet of fish from the western Barents sea (first-year ice) consisted mainly of copepods (Calanus finmarchicus, Calanus glacialis) and the hyperiid amphipod Parathemisto libellula. Fish collected north of the Svalbard archipelago (multi-year ice) had a more diverse diet, in which P. libellula and the sympagic amphipod Apherusa glacialis contributed more to the total diet biomass than copepods.
The nature of the substratum is a fundamental factor determining the types of organisms and commu... more The nature of the substratum is a fundamental factor determining the types of organisms and communities found in many terrestrial and benthic habitats. The extent to which this is true in extreme environments was investigated using bryozoan assemblages as model organisms in an Arctic fjord (Kongsfjorden 79°N, 12°E) in summer 2001 using SCUBA. Twenty-seven substrate samples of 0.25 m2 were taken at 10 m depth from the inner glacial basin to the mouth of the fjord. Multivariate analyses revealed four different bryozoan assemblages. The sea floor of the inner basin of Kongsfjorden near the glacial fronts was characterized by low diversity and dominance of the ctenostome species Alcyonidium disciforme Smitt. Highest richness and diversity occurred on rock substratum with mean size >10 cm2, on which the most common species was the pioneer Harmeria scutulata Busk (abundance: 15%). On smaller rocks with mean size 2, the runner-like pioneer species Electra arctica Borg comprised most individuals of the assemblage (98%). Yet another pioneer, Celleporella hyalina Linnaeus, was the most abundant species (49%) on substratum dominated by algae. Thus, in each habitat type, pioneers dominated but different species and to different extents. There was much variation in species composition and abundance within assemblages of heterogeneous habitats, and this study emphasizes the importance of microhabitats and physical conditions. Heterogeneity was evident at scales of
The object of the present investigation was to map the distribution and abundance of sympagic fau... more The object of the present investigation was to map the distribution and abundance of sympagic fauna (= ice fauna) (>350 μm) within the perennial sea ice zone near Svalbard and to study relations between the sympagic fauna and the age and history of its ice substrate. The sampling took place in July/August 1986 and September 1988 using SCUBA-operated sampling gear (suction samplers, plankton nets with especially designed frames for sampling at the sea-ice/seawater interface, and underwater cameras). The amphipods Apherusa glacialis, Onisimus sp., and Gammarus wilkitzkii were the most conspicuous sympagic species both years. Scattered individuals of the amphipods Gammaracanthus loricatus, Weyprechtia penguis and the polychaete Harmathoinae indet. were also recorded. A. glacialis was the most numerous and contributed near 65% of the collected specimens in both years, with a maximum density exceeding 2000 individuals/m2. However, G. wilkitzkii was on average larger, and contributed most to the biomass (1986: 80%; 1988: 77%). The average biomass of sympagic fauna in 1986 and 1988 was estimated to be 4.7 g/m2 and 8.3 g/m2 respectively. Biomass values reported here are ten to hundred times higher than what is found within the seasonal sea ice zone. Autochthonous sympagic species, like A. glacialis, Onisimus sp. and G. wilkitzkii, have a permanent association with ice. The seasonal sea ice zone will thus have to be recolonized every year resulting in lower densities compared to multiyear ice. It is suggested that the speed of the ice leaving the Polar Basin through the Fram Strait is too high for the sympagic fauna to remain its position in the sea ice zone. The result is an annual loss in the order of 7*105 tons of sympagic fauna from the perennial sea ice zone.
The sympagic fauna (= sea ice fauna) of the Barents Sea was investigated on nine (2–5 weeks) crui... more The sympagic fauna (= sea ice fauna) of the Barents Sea was investigated on nine (2–5 weeks) cruises in the period 1983–1988. The amphipods Apherusa glacialis, Onisimus sp. and Gammarus wilkitzkii were the most conspicuous and abundant invertebrate species associated with the ice. Mean biomass-values ranged from 0 to about 2 g/m2, and were less than 0.001 g/m2 in five of the nine cruises. Apherusa glacialis, Onisimus sp. and Gammarus wilkitzkii are regarded as autochthonous sympagic species, and as such dependent upon a permanent ice cover. Allochthonous sympagic species were few and without significant importance. The variations in species abundance and biomass were believed to be closely connected to the age and drift-history of the ice. The density of the sympagic fauna increases as a result of increasing influx of ice into the Barents Sea from the Arctic Ocean. Density of the sympagic fauna were believed to increase with decreasing distance to the multiyear/first-year ice boundary. A. glacialis was found further away from the spreading centers and in higher numbers than the other sympagic species due to its greater motility. No day-night variations in the occurrences of the sympagic fauna were recorded.
The distribution of juvenile benthic invertebrates with respect to their abiotic environment was ... more The distribution of juvenile benthic invertebrates with respect to their abiotic environment was investigated at four locations along a gradient in Kongsfjorden (79°N, 12°E), Spitsbergen, in September 1997. Heavy discharge of inorganic sediments released by the three glaciers was expected to be one of the main structuring factors of benthic communities in the fjord. Juveniles of 76 species/families are identified. Total abundance increases with distance from the fjord head due to the dominance of opportunistic polychaetes, while diversity is highest close to the glacier. Juvenile polychaetes are the most abundant taxon over all stations (92%), followed by bivalves, crustaceans and others. Polychaetes also provide most species (55%) and are the dominant taxon at every station. Their abundance is highly correlated with total organic carbon, indicating that most of them are deposit feeders. Young crustaceans rapidly decrease towards the fjord mouth, probably due to stronger bottom currents. Even though young oligochaetes are exclusively found near the glacier, no species seem to be well adapted to the high sedimentation rate close to the glacier. Juvenile suspension-feeding bivalves seem to be less disturbed by glacial discharge but appear to be more vulnerable to currents on the more exposed sites. The importance of deposit feeders and carnivores increases towards the outer stations. Non-metric multidimensional scaling confirms the distinct gradient in community composition along the fjord. Coupling the biotic data to abiotic factors (depth, bottom-water salinity, bottom-water temperature, sediment grain size and sedimentation rate) using canonical correspondence analysis revealed that hydrographic factors are more responsible for the structuring of the benthic juvenile community at the shallow stations close to the glacier (except the station directly at the glacier). At the outer deeper stations, sediment grain size and related properties may play a more important role.
We describe the summer diets of four seabird species, Kittiwake (Rissa tridactyla), Little Auk (A... more We describe the summer diets of four seabird species, Kittiwake (Rissa tridactyla), Little Auk (Alle alle), Black Guillemot (Cepphus 9rylle) and Brfinnich's Guillemot (rJria lomvia) collected in sea-ice-covered waters near SwLlbard. Birds collected in an area filled with young sea-ice, within the seasonal sea-ice zone, were compared with birds collected from the perennial sea-ice zone dominated by multiyear ice. Pelagic Crustacea and fish dominated tt~e diet of birds feeding in young ice, while sympagic Crustacea and fish were most important in the diet of birds feeding in multiyear ice. Boreogadus saida was the most important fish food item. B. Saida was present in the ice in both areas, while sympagic Crustacea were lacking in the area filled with young ice. Important food items in young k:e were B. saida (Black Guillemots and Kittiwakes), Caianus sp. (Little Auks) and Pandalusborealis (Brfinnich's Guillemot). B. saida (Black Guillemots, Kittiwakes, Brfinnich's Guillemots), Gammarus wilkitzkii (Brfinni~:h's Guillemot, Black Guillemot) and Apherusa glacialis (Little Auk) were most important in multiyear ice.
Svalbard bryozoan communities were investigated along a depth range from the surface to 296 m bet... more Svalbard bryozoan communities were investigated along a depth range from the surface to 296 m between the inner glacial fronts and fjord mouths during 2001 and 2002. The main study area was Kongsfjorden (79°N, 12°E). A total of 137 taxa of bryozoans were identified: 108 to species, 24 to genus, 3 to family, 1 to order and 1 to phylum level. Cluster and multidimensional scaling analyses revealed four distinct assemblages of bryozoans: shallow (0-40 m; 68 taxa), deep (40-296 m; 80 taxa), inner fjordic (three taxa) and an assemblage found on small stones in shallow waters (nine taxa). The inner fjordic assemblage was recorded from the front of tidal glaciers extending about 10 km out into the fjord. In terms of abundance, Celleporella hyalina Linnaeus dominated in shallow areas (18%), Hippothoa arctica Kluge (55%) in deep water, Alcyonidium disciforme Smitt (86%) proximate to glaciers fronts and Electra arctica Borg on small stones (98%).
Arctic ice amphipods are part of the sympagic macrofauna in the Marginal Ice Zone of the northern... more Arctic ice amphipods are part of the sympagic macrofauna in the Marginal Ice Zone of the northern Barents Sea and represent an important link from lower to higher trophic levels in some Arctic marine food chains. The species diversity in this area (1995/1996) consisted of four species: Gammarus wilkitzkii, Apherusa glacialis, Onisimus nanseni and Onisimus glacialis. The larger ice amphipod, G. wilkitzkii, was the most abundant with the highest biomass (>90%), whereas A. glacialis was abundant, but contributed little to the total biomass (<4%). The other two species were found only in small numbers. Both abundance and biomass of ice amphipods decreased along a latitudinal gradient from north to south across the Marginal Ice Zone. Their distribution was also related to the under-ice topography with regard to mesoscale structures (edge,¯at area, dome and ridge). Overall, the abundance and biomass on ridges were much higher in comparison to other mesoscale structures, although edges also showed high abundance, but low biomass. The large G. wilkitzkii was consistently abundant on ridges. The small A. glacialis was predominately associated with edges, but also showed high numbers in dome-shaped areas. The Onisimus species were present in low numbers at all structures, and their biomass contributed <10% on any one structure. The reasons for dierent distribution patterns of the dominant amphipod species under Arctic sea ice are probably related to dierent requirements of the species, especially for food, shelter and physiological conditions.
Zooplankton samples were collected in January 1993 o Dronning Maud Land along a transect from ope... more Zooplankton samples were collected in January 1993 o Dronning Maud Land along a transect from open waters to the marginal ice zone close to the Antarctic ice shelf. Thysanoessa macrura was caught in open waters while Calanoides acutus and Calanus propinquus were mainly sampled between ice¯oes in the marginal ice zone. The``ice-krill'' Euphausia crystallorophias was found over the shelf directly associated with ice¯oes. T. macrura had a lipid content up to 36% of its dry weight with the dominant lipid class, wax ester, accounting for 45±50% of the total lipid. The predominance of 18:1 fatty alcohols is the striking characteristic of the wax esters. Small specimens of E. crystallorophias had lipid levels up to 26% of their dry weight with, unexpectedly, triacylglycerols being the dominant lipid (up to 41% of total lipid). The small levels of wax esters in these animals (3±6% of total lipid) had phytol as a major constituent. Large specimens of E. crystallorophias had up to 34% of their dry weight as lipid, with wax esters (47% of total lipid) dominated by 16:0 and 14:0 fatty alcohols as the major lipid. Calanus propinquus had lipid levels of up to 34% of their dry weight, with triacylglycerols (up to 63% of total lipid) being the dominant lipid. High levels of 22:1 (n-9) fatty acid were present in the triacylglycerols. Calanoides acutus had lipid levels up to 35% of the dry weight with wax esters accounting for up to 83% of total lipid. High levels of (n-3) polyunsaturated fatty acids were recorded with 20:5(n-3), 22:6(n-3) and 18:4(n-3) being the dominant moieties. On the basis of their lipid compositions we deduce that: (1) Calanoides acutus is the strictest herbivore among the four species studied, heavily utilizing the typical spring bloom; (2) T. macrura is essentially omnivorous, probably utilizing the less de®ned bloom situations found in oceanic waters; (3) E. crystallorophias is an omnivore well adapted to utilize both a bloom situation and to feed on ice algae and micro-zooplankton associated with the ice; (4) Calanus propinquus seems to be the most opportunistic feeder of the four species studied, probably grazing heavily on phytoplankton during a bloom and, during the rest of the year, feeding on whatever material is available, including particulates,¯agellates and other ice-associated algae. We conclude that the dierent biochemical pathways generating large oil reserves of dierent compositions, enabling species to utilize dierent ecological niches, are major determinants of biodiversity in polar zooplankton.
Gammarus wilkitzkii, Apherusa glacialis, Onismus nanseni, Onismus glacialis, Boreogadus saida, Pa... more Gammarus wilkitzkii, Apherusa glacialis, Onismus nanseni, Onismus glacialis, Boreogadus saida, Parathemisto libellula and Calanus hyperboreus, collected in late June in the Barents Sea marginal ice zone, contained substantial levels (28±51% of the dry mass) of total lipid, the highest levels (51% and 41% respectively) being in A. glacialis and C. hyperboreus. Neutral lipids were present in greater amounts than polar lipids in all species. Triacylglycerols were major neutral lipids in A. glacialis, G. wilkitzkii and O. nanseni; triacylglycerols and wax esters were present in similar amounts in O. glacialis; higher levels of wax esters than triacylglycerols occurred in P. libellula; wax esters greatly exceeded triacylglycerols in C. hyperboreus, the opposite being true for B. saida. Diatom fatty acid markers were prominent in the triacylglycerols of G. wilkitzkii, O. nanseni, O. glacialis and, particularly, of A. glacialis; 20:1(n-9) and 22:1(n-11) moieties were abundant in wax esters of G. wilkitzkii, O. nanseni, O. glacialis, P. libellula and C. hyperboreus, and in triacylglycerols of B. saida. We deduce that A. glacialis feeds mainly on ice algae and phytodetritus, G. wilkitzkii and the Onismus spp. feed on calanoid copepods as well as ice algae, whereas P. libellula and especially B. saida feed extensively on calanoid copepods.
The distribution of juvenile benthic invertebrates with respect to their abiotic environment was ... more The distribution of juvenile benthic invertebrates with respect to their abiotic environment was investigated at four locations along a gradient in Kongsfjorden (79°N, 12°E), Spitsbergen, in September 1997. Heavy discharge of inorganic sediments released by the three glaciers was expected to be one of the main structuring factors of benthic communities in the fjord. Juveniles of 76 species/families are identified. Total abundance increases with distance from the fjord head due to the dominance of opportunistic polychaetes, while diversity is highest close to the glacier. Juvenile polychaetes are the most abundant taxon over all stations (92%), followed by bivalves, crustaceans and others. Polychaetes also provide most species (55%) and are the dominant taxon at every station. Their abundance is highly correlated with total organic carbon, indicating that most of them are deposit feeders. Young crustaceans rapidly decrease towards the fjord mouth, probably due to stronger bottom currents. Even though young oligochaetes are exclusively found near the glacier, no species seem to be well adapted to the high sedimentation rate close to the glacier. Juvenile suspension-feeding bivalves seem to be less disturbed by glacial discharge but appear to be more vulnerable to currents on the more exposed sites. The importance of deposit feeders and carnivores increases towards the outer stations. Non-metric multidimensional scaling confirms the distinct gradient in community composition along the fjord. Coupling the biotic data to abiotic factors (depth, bottom-water salinity, bottom-water temperature, sediment grain size and sedimentation rate) using canonical correspondence analysis revealed that hydrographic factors are more responsible for the structuring of the benthic juvenile community at the shallow stations close to the glacier (except the station directly at the glacier). At the outer deeper stations, sediment grain size and related properties may play a more important role.
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Papers by Ole Lønne