Trends in benthic macrofaunal populations, seasonal sea ice persistence, and bottom water temperatures in the bering strait region

• Published in: Oceanography
• Main Authors: Grebmeier, Jacqueline M., Frey, Karen E., Cooper, Lee W., Kędra, Monika
• Format: Text
• Language: unknown
• Published: Clark Digital Commons 2018
• Subjects: benthic macrofaunal populations; sea ice; marine ecosystems; Bering Strait; Chukchi Sea; Climate; Oceanography; Arctic; Lawrence Island; Chukchi; Sea ice; St Lawrence Island
• Online Access: https://commons.clarku.edu/faculty_geography/199; https://doi.org/10.5670/oceanog.2018.224; https://commons.clarku.edu/context/faculty_geography/article/1198/viewcontent/GeogFacWorks_Frey_TrendsBenthic_2018.pdf

Recent declines in sea ice extent and warming seawater temperatures in the Arctic have the potential to impact regional and pan-Arctic marine ecosystems. To investigate marine biological response to these key drivers and other environmental factors, we undertook a robust trend analysis of benthic macrofaunal populations and environmental drivers in the Bering Strait region. Our focus was on the waters of the northern Bering and southern Chukchi Seas, which are shallow (m) and seasonally productive, with strong pelagic-benthic coupling between water-column-derived organic matter and the seafloor. Studies indicate that both in situ production and advection of upstream phytodetritus support persistent biologically productive regions, termed hotspots, in the greater Bering Strait region. The benthic marine ecosystem is dominated by macroinvertebrates (e.g., clams, polychaetes, and amphipods) that in turn serve as food resources for diving mammals and seabirds, thus allowing for changes to cascade strongly through the food web from prey to predator. During our study, the persistence of seasonal sea ice significantly declined; trend analyses indicate both earlier sea ice breakup and later fall freeze-up in recent years. When combined with warming seawater temperatures in the region, these changes have ramifications for water column processes that influence benthic faunal biomass and composition, which can transfer to upper trophic level predators. We studied these changes by evaluating time series sites in three benthic biomass hotspots starting in 1998 (Southeast Chukchi Sea region), 1999 (Chirikov Basin region), and 2000 (St. Lawrence Island Polynya region). We present these data within a broader evaluation of benthic biomass results from prior cruises dating as early as the 1970s. The current study focuses on the period 1998–2015 at sites occupied annually each July using CCGS Sir Wilfrid Laurier. Since 2010, these time series sites have become part of the international Distributed Biological Observatory (DBO), a ...