On the direct impact of ice on marine benthic communities, a review

By J. Gutt. Polar Biology, 2001

340 citations recorded by the source corpus.

Subfields: Global and Planetary Change, Oceanography

View Paper: https://www.semanticscholar.org/paper/bbbd7d5b76ab626b112d79b094d2aca105909712

How researchers see this paper

The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.

In Global and Planetary Change

1. L. Peck
2. D. Barnes
3. A. Clarke
4. Huw Griffiths
5. D. Piepenburg
6. J. Gili
7. R. Aronson
8. D. Blake

In Oceanography

1. L. Peck
2. A. Clarke
3. D. Barnes
4. C. Wiencke
5. Huw Griffiths
6. K. Bischof
7. D. Piepenburg
8. J. Gili

Citations in the corpus

• Antarctic sessile marine benthos: colonisation and growth on artificial substrata over three years (2006, background): “Third, the gradient of decreasing physical disturbance by ice with increasing depth is the principal factor determining sessile assemblage structure in nearshore waters (Dayton 1990, Arntz et al. 1994, Barnes 1999, Gutt 2001).”
• The Antarctic-Magellan connection: Macrobenthos ecology on the shelf and upper slope, a progress report (2005, background): “Despite its immediate destructive effects, it is evident now that iceberg scouring enhances diversity whereas glaciers cause faunal impoverishment (Gutt, 2001).”
• Antarctic marine benthic diversity: patterns and processes (2008, background): “Work on iceberg disturbance has shown that intermittent catastrophic disturbancewill affect the composition, distribution and abundance of faunal assemblages (Gutt, 2001; Gutt and Piepenburg, 2003), and it seems unlikely from current knowledge that glacio-marine processes will have eradicated the en”
• The spatial structure of Antarctic biodiversity (2014, background): “Ice scour is a key element of marine disturbance in Antarctica (Table 6 [see also Gutt 2001, Gutt and Starmans 2001, Brown et al. 2004, Thrush et al. 2006]).”
• Life strategy, ecophysiology and ecology of seaweeds in polar waters (2007, background): “Icebergs can run aground in the Antarctic down to 600 m depth (Gutt 2001).”
• Recent research on Arctic benthos: common notions need to be revised (2005, background): “At certain exposed locations, they cover 50% of the seabed, indicating that up to 7% of the total area of the Antarctic shelves (<350 m) might be affected by grounding impacts within the past 20 years (Gutt 2001).”
• Zoobenthic biodiversity, biomass and abundance at Adelaide Island, Antarctica (2003, background): “Intermediate disturbancepromoted diversity (Connell 1978, Huston 1979) has rarely been invoked to systems at continent spatial scale (but see Gutt 2001), or at geological timescale, but there is no theoretical barrier why the same processes should not work at higher scales.”
• Evolution and diversity of the benthic fauna of the Southern Ocean continental shelf (2004, background): “The intensity and frequency of these scours are major features dictating assemblage structure and population dynamics in the Antarctic continental shelf benthos (Gutt 2000, 2001, Gutt & Starmans 2001, Gutt & Piepenburg 2003).”
• Reproduction in cold water: paradigm changes in the 20th century and a role for cidaroid sea urchins (2004, background): “In addition, once cooled, Antarctic seas would be subject to ice disturbance (Gutt, 2001), and pieces of anchor ice or grounded shelf ice could lift benthic organisms off the bottom and transport them to distant locations (Picken, 1980).”
• Microplastics in the Antarctic marine system: An emerging area of research. (2017, background): “The impacts of ice scour, together with advection, result in the resuspension of sediments (Barnes and Souster, 2011; Gutt, 2001), and potentially any microplastics within them, which may increase the likelihood of them being ingested by benthic taxa in coastal areas.”
• Soft-bottom macrobenthic faunal associations and factors affecting species distributions in an Arctic glacial fjord (Kongsfjord, Spitsbergen) (2004, background): “The effect of icebergs on sediments may result from direct scouring or from resuspension and sediment transport caused by water circulation around an iceberg (Peck et al. 1999; Gutt 2001).”