Analyzing Pacific-Arctic ecosystems in a warming climate
Receding sea ice and increased ocean temperatures are driving shifts in marine ecosystems, especially within the Arctic-Pacific seas. These changes are affecting a variety of ecosystem dynamics, from primary productivity to benthic species density, which could lead to irreversible tipping points for the Arctic system.
The Distributed Biological Observatory (DBO) is a change detection array extending from the northern Bering Sea to the Barrow Canyon region, specifically at the junction of the Chukchi and Beaufort seas. The array additionally extends eastward into the Canadian Beaufort Sea for a subset of measurements (see below figure). Since 2010 and spanning six countries, the DBO has provided a framework to coordinate sampling and analytical efforts linking biological changes to physical drivers, such as sea ice melt or warming surface temperatures. Datasets collected include key water column parameters (stable isotopes of oxygen in water, phytoplankton species composition), sediment parameters (organic carbon and nitrogen content, grain size, stable isotope C and N content of organic matter, and whole core metabolism measurements), and benthic macrofaunal composition and biomass.
The goals of the project are to determine hydrographic and sediment characteristics that influence macrofaunal communities and ecosystem function through field and synthesis studies. The field cruises also contribute to related investigations of harmful algal blooms in the Arctic. These blooms have trophic impacts that are critical for assessing food security in the region. Exploratory work is also assessing the genomic composition of dominant benthic animals for applications for food tracing, and other food web studies.