Invertebrate community assembly along proglacial chronosequences in the high Arctic

By I. Hodkinson, S. Coulson, N. Webb. 2004

139 citations recorded by the source corpus.

Subfields: Atmospheric Science, Ecology

View Paper: https://www.semanticscholar.org/paper/97e85793401532bd200f3c6a592913a5a982360e

How researchers see this paper

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

In Atmospheric Science

1. A. Milner
2. Karin Hohberg
3. K. Klanderud
4. Sigmund Hågvar
5. G. Velle
6. Peter Convey

In Ecology

1. L. Brown
2. A. Milner
3. D. Peltzer
4. David A. Wardle
5. E. Doblas-Miranda
6. L. Füreder
7. G. Yeates
8. Sigmund Hågvar

Citations in the corpus

• The terrestrial and freshwater invertebrate biodiversity of the archipelagoes of the Barents Sea; Svalbard, Franz Josef Land and Novaya Zemlya (2014, background): “Polar (Arctic and Antarctic) ecosystems are considered to be particularly valuable for studies addressing such fundamental questions of ecosystem function, providing examples across a wide range of levels of assemblage structure (Hodkinson et al., 2003, 2004; Adams et al., 2006; Post et al., 2009).”
• Arctic biodiversity assessment : status and trends in arctic biodiversity (2013, background): “For example, a study of the progressive colonization of the glacier foreland of Midtre Lovénbreen, Svalbard, with respect to elapsed time since exposure, showed that colonization by pioneer species is rapid, but that it may take up to 2000 years for the full complement of species found in the surrou”
• Colonization and development of an Alaskan stream community over 28 years (2008, background): “Hodkinson et al. (2004) considered this succession to be deterministic and linked to plant community and soil development, with little further change in invertebrate communities after 50 years (Kaufmann 2001).”
• Active dispersal of oribatid mites into young soils (2012, background): “, 2008) and in the initial phase of primary succession, they facilitate plant succession as well as the colonization by other organisms (Hodkinson et al., 2004).”
• Vulnerability of alpine stream biodiversity to shrinking glaciers and snowpacks (2007, background): “Although meltwater thresholds for individual species have not previously been demonstrated, they must be related to glacier retreat in similar ways to which successional sequences occur in aquatic and terrestrial systems following deglaciation (e.g. Milner et al., 2000; Hodkinson et al., 2004).”
• Effect of simulated environmental change on alpine soil arthropods (2009, background): “In a proglacial area in the high Arctic, Hodkinson et al. (2004) found that heat extraction was more efficient than O’Connor’s (1962) wet extraction for terrestrial larvae of Chironomidae, but the general value of this comparison is uncertain.”
• Changes in the community structure and diversity of soil invertebrates across the Franz Josef Glacier chronosequence (2008, background): “These include studies on communities of microorganisms (Tscheko et al., 2003), mycorrhizal fungi (Jumpponen et al., 2005), nematodes (Yeates, 1971; Wasilewska, 1994), microarthropods (Chauvat et al., 2003; Hodkinson et al., 2004) and earthworms (Scheu, 1992).”