Death in southern Patagonian fjords: Copepod community structure and mortality in land- and marine-terminating glacier-fjord systems

Abstract

Abstract Glacial retreat at high latitudes has increased significantly in recent decades associated with global warming. Along Chile s Patagonian fjords, this has promoted increases in freshwater discharge, vertical stratification, and the input of organic and inorganic particles to fjords. In addition, it has modified the water chemistry [i. e. nutrient stoichiometry] and its associated biota. This study evaluates the effect of deglaciation in high-latitude fjords (54°S) on copepod survival and how this might affect the export of particulate organic carbon to the benthos. We selected two contrasting fjord systems in terms of their geomorphology and the quality and quantity of freshwater contributions: (a) Pia Fjord, with marine-terminating glaciers, and (b) Yendegaia Fjord, with land-terminating-glaciers. Both are located along the Beagle Channel (54°S), southern Chilean Patagonia. These two fjords differed significantly in phytoplankton and copepod biomass. Whereas Pia Fjord showed high chlorophyll-a concentration (7\u202fmg\u202fChl-a\u202fm−3) and copepod abundance (970\u202find.\u202fm−3), in Yendegaia Fjord, the biomass was very low for both autotrophs ( 1000\u202fµm). The presence of carcasses was better explained by the amount of suspended particulate inorganic matter in the water column than by salinity. The contribution of dead copepods to the vertical carbon flux was