LONG‐TERM CHANGES IN THE MACROALGAL VEGETATION OF THE INNER GULLMAR FJORD, SWEDISH SKAGERRAK COAST1

By B. K. Eriksson, G. Johansson, P. Snoeijs. 2002

122 citations recorded by the source corpus.

Subfields: Ecology, Oceanography

View Paper: https://www.semanticscholar.org/paper/662a1228057bbbcd8b004ca6da9450c7efd8a252

How researchers see this paper

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

In Ecology

1. T. Wernberg
2. I. Muxika
3. S. Connell
4. Gary A. Kendrick
5. Á. Borja
6. F. Moy
7. D. Balata
8. Sonia K. Gorgula

In Oceanography

1. T. Wernberg
2. I. Muxika
3. S. Connell
4. Á. Borja
5. Gary A. Kendrick
6. D. Balata
7. F. Moy
8. L. Piazzi

Citations in the corpus

• Biomass, diversity and production of rocky shore macroalgae at two nutrient enrichment and wave action levels (2010, background): “Increased nutrient enrichment due to human activities is today commonly perceived as a major contributor to the deterioration of coastal ecosystems worldwide including vast structural and functional ecosystem changes (Nixon 1995; Schramm 1999; Cloern 2001; Eriksson et al. 2002).”
• Testing a new classification of morphological functional groups of marine macroalgae for the detection of responses to stress (2011, background): “Because of their sessile condition, benthic macroalgae integrate the effects of long-term exposure to pollutants resulting in a shift of the structure of assemblages related to a decrease of the most sensitive species and its replacement by highly tolerant species ( Eriksson et al. 2002; Gorgula an”
• Long-term recovery of soft-bottom benthos following urban and industrial sewage treatment in the Nervión estuary (southern Bay of Biscay) (2006, background): “…of both the community (as an indicator of the level of biological organisation) and the benthos (as an indicator of the biotic component) in monitoring programmes has been justified largely for temperate coastal areas (Clarke & Green 1988, Warwick 1993, Clarke & Warwick 1994, Eriksson et al. 2002).”
• Large-scale shift from sugar kelp (Saccharina latissima) to ephemeral algae along the south and west coast of Norway (2012, background): “In the Skagerrak region, eutrophication and increased sedimentation on rocky bottoms have been found consistent with long-term changes in both macroalgae diversity and depth distribution (Pedersén & Snoeijs 2001; Eriksson et al. 2002).”
• Expansive covers of turf-forming algae on human-dominated coast: the relative effects of increasing nutrient and sediment loads (2004, background): “This pattern is frequently observed on the world’s temperate coasts (Benedetti-Cecchi et al. 2001) and is variously considered to be a result of enhanced concentrations of nutrients (Worm et al. 2000b; Eriksson et al. 2002 ) or rates of sediment deposition (Eriksson et al. 2002; Airoldi 2003).”
• Modification of the physical environment by an Ecklonia radiata (Laminariales) canopy and implications for associated foliose algae (2005, background): “In this study we focus on light, sediment cover and water motion because these three factors are affected by macroalgal canopies and have been identified as important to the organization of marine communities (light: Kennelly 1989; Irving and Connell 2002; Toohey et al. 2004; sediments: Kendrick 199”
• European seaweeds under pressure: Consequences for communities and ecosystem functioning (2015, background): “Furthermore, the decrease of depth limits of macroalgae and disappearance of characteristic zonation patterns (Breuer and Schramm, 1988; Eriksson et al., 2002; Middelboe and Sand-Jensen, 2000; Middelboe et al., 1998) due to reduced light penetration is an important consequence of eutrophication that”