Long-term studies of the marine ecosystem along the west Antarctic Peninsula

Abstract

Articles in this volume focus on longer-term studies of the marine ecosystem of the continental shelf west of the Antarctic Peninsula, principally by the Palmer, Antarctica Long- Term Ecological Research project (Ross et al., 1996; Ducklow et al., 2007). There is a rich history of oceanographic and ecological research in the Bellingshausen Sea region and on the continental shelf dating back to the 19th and early 20th centuries (El-Sayed, 1996). The modern era of scientific research started with the British Discovery Investigations of 1925-37 (Hardy, 1967), and included classic studies of phytoplankton (Hart, 1934) and krill (Marr, 1962). Hart’s report presciently suggested primary producers could be limited by iron availability. El-Sayed (1996) dissects the subsequent history of oceanographic research up to the advent of the Southern Ocean GLOBEC (Hofmann et al., 2001; Hofmann et al., 2004) and JGOFS (Anderson and Smith Jr., 2001) programs. The period from the 1970’s to the mid-90’s was dominated by expeditionary and process-level studies of particular regions and processes extending over a few seasons to a few years at most. The Research on Antarctic Coastal Ecosystem Rates (RACER) Program (Huntley et al., 1991; Karl, 1991) is the outstanding example of this mode of research, having focused on determination of key rate processes as a new approach to understanding ecosystem dynamics (Karl et al., 1991a; Karl et al., 1991b). RACER was a direct predecessor and major influence on Palmer LTER, GLOBEC and JGOFS. What was lacking in Antarctic waters, as in most other regions and ocean provinces were sustained, long-term observations of a variety of ocean properties and rates, conducted in the context of hypothesis-driven, experimental science (Ducklow et al., 2008a). The creation of the US LTER Network in 1980 (Magnuson, 1990) made this possible.