2010
DOI: 10.1016/j.marenvres.2009.08.005
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Temporal variability of benthic communities in an Alaskan glacial fjord, 1971–2007

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Cited by 26 publications
(24 citation statements)
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“…Benthic diversity and biomass can change significantly from the outer to the inner parts of Arctic and Subarctic fjords (Kendall and Aschan 1993;Holte and Oug 1996;Włodarska-Kowalczuk et al 2005;Blanchard et al 2010). The chronic disturbance associated with glacial activity is especially visible in the shallow areas located close to the glacial terminus (Włodarska-Kowalczuk et al 1998;Włodarska-Kowalczuk and Pearson 2004;Siciński et al 2012); however, this influence can be very strong to as deep as 100 m (Siciński 2004).…”
Section: Introductionmentioning
confidence: 99%
“…Benthic diversity and biomass can change significantly from the outer to the inner parts of Arctic and Subarctic fjords (Kendall and Aschan 1993;Holte and Oug 1996;Włodarska-Kowalczuk et al 2005;Blanchard et al 2010). The chronic disturbance associated with glacial activity is especially visible in the shallow areas located close to the glacial terminus (Włodarska-Kowalczuk et al 1998;Włodarska-Kowalczuk and Pearson 2004;Siciński et al 2012); however, this influence can be very strong to as deep as 100 m (Siciński 2004).…”
Section: Introductionmentioning
confidence: 99%
“…Weathered petroleum enters the fjord via a diffuser pipeline through which treated ballast water (taken from incoming tankers and treated onshore) is discharged. Prior studies demonstrated limited effects on benthic fauna from short-term increases in sediment hydrocarbon at a shallow station adjacent to the point of discharge for treated ballast water while no effects were noted from hydrocarbons at deep sampling locations (Blanchard et al 2002(Blanchard et al , 2010. The quantity of treated ballast water discharged into the fjord has declined over the study period but associated changes in benthic fauna have not been observed (Blanchard et al 2002;Payne et al 2008).…”
Section: Introductionmentioning
confidence: 85%
“…The fjord has two sills (at 120 and 200 m depth) which limit bottom-water circulation and a relatively flat bottom reaching a depth of 230 to 250 m. The residence time of mid-depth water is estimated as 40 days due to a slow, counter-clockwise circulation (Colonell et al 1988). Macrofaunal abundance and biomass are relatively low and spatial trends in community structure are associated with a gradient in sediment deposition and grain size within the fjord (Feder and Matheke 1980;Feder and Jewett 1988;Blanchard et al 2010). Oily ballast water from tankers is treated onshore to remove hydrocarbons through physical, chemical, and biological treatment phases (Shaw and Hameedi 1988).…”
Section: Study Areamentioning
confidence: 99%
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“…Environment-growth relationships were most common with 2-year lags or during the current summer of fish growth. Again, a mechanism involving the Kelp Greenlings' prey may be responsible, as warmer conditions are associated with increased abundance (Blanchard et al 2010), growth (Neuparth et al 2002;Black et al 2009;Stoner et al 2010;Helser et al 2012), development (Shirley et al 1987;Hoegh-Guldberg and Pearse 1995), and reproduction (Hines 1982;Neuparth et al 2002) of benthic invertebrates.…”
Section: Kelp Greenlings In the Alaska Coastal Currentmentioning
confidence: 99%