Gérald Darnis
Université Laval, Biologie, Graduate Student
Research Interests:
ABSTRACT We investigated the seasonal vertical migration of seven dominant arctic copepod species from October 2007 to July 2008 in Amundsen Gulf. The large herbivore Calanus hyperboreus resided in the deep Atlantic Layer from December to... more
ABSTRACT We investigated the seasonal vertical migration of seven dominant arctic copepod species from October 2007 to July 2008 in Amundsen Gulf. The large herbivore Calanus hyperboreus resided in the deep Atlantic Layer from December to mid-April, rapidly invaded the surface layer at the onset of the phytoplankton bloom in early May, and started its descent to overwintering depth in July. C. glacialis overwintered at shallower depths than C. hyperboreus, moved into the surface layer in early April as ice algae bloomed, and remained in the subsurface chlorophyll maximum (SCM) until late July. The small omnivore Oithona similis slowly rose into the Polar-Mixed Layer from February to April, reaching the ice-water interface in early April as ice algae developed. The very small Triconia borealis associated with C. hyperboreus in the Atlantic Layer from October to April. The mesopelagic omnivores Metridia longa and Microcalanus pygmaeus could be characterized as mid-depth interceptors, feeding on microzooplankton in winter, the upward flux of C. hyperboreus eggs in late winter-early spring, and on the rain of microalgae in spring-summer. The epipelagic Pseudocalanus spp. distributed in a narrow band centered around 50 m from October to April, then descended under the SCM from May to July. Copepods generally avoided the lens of warm (2-8A degrees C) surface water in summer, but readily migrated across the -1.7A degrees C to +0.3A degrees C gradient from the Polar-Mixed Layer to the Atlantic Layer. The different patterns of seasonal migrations dictated the different temperature regimes experienced over the year by each species and copepodite stage.
Research Interests:
Major pathways of biogenic carbon (C) flow are resolved for the planktonic food web of the flaw lead polynya system of the Amundsen Gulf (southeast Beaufort Sea, Arctic Ocean ) in spring-summer 2008. This period was relevant to study the... more
Major pathways of biogenic carbon (C) flow are resolved for the planktonic food web of the flaw lead polynya system of the Amundsen Gulf (southeast Beaufort Sea, Arctic Ocean ) in spring-summer 2008. This period was relevant to study the effect of climate change on ...
Research Interests: Geology and Oceanography
Research Interests:
... Ingestion estimates based on the measurement of fae-cal pellet production rates (FPP), combined with anal-ysis of the egested volume ... 5 females in good condition, judged by normal swimming behaviour and escape response, were... more
... Ingestion estimates based on the measurement of fae-cal pellet production rates (FPP), combined with anal-ysis of the egested volume ... 5 females in good condition, judged by normal swimming behaviour and escape response, were transferred into incubation chambers (0.9 l ...