2002
DOI: 10.1016/s0079-6611(02)00007-1
|View full text |Cite
|
Sign up to set email alerts
|

Sediment distribution patterns on the Galicia-Minho continental shelf

Help me understand this report

Search citation statements

Order By: Relevance

Paper Sections

Select...
3
1
1

Citation Types

2
69
1
1

Year Published

2005
2005
2023
2023

Publication Types

Select...
7
1
1

Relationship

0
9

Authors

Journals

citations
Cited by 98 publications
(73 citation statements)
references
References 13 publications
2
69
1
1
Order By: Relevance
“…Moreover, grain size was relatively smaller at Station I11 than at Stations I and 11, indicating that sediment at Station I11 was more easily resuspended. The poor sorting of sediment grain size at Station 111 (2.0) also indicated frequent resuspension of the sediment as reported in previous studies (Dias et al 2002, Christiansen et al 1993, Brassard and Morris 1997.…”
Section: Resuz=ts and Discussionsupporting
confidence: 80%
“…Moreover, grain size was relatively smaller at Station I11 than at Stations I and 11, indicating that sediment at Station I11 was more easily resuspended. The poor sorting of sediment grain size at Station 111 (2.0) also indicated frequent resuspension of the sediment as reported in previous studies (Dias et al 2002, Christiansen et al 1993, Brassard and Morris 1997.…”
Section: Resuz=ts and Discussionsupporting
confidence: 80%
“…Desroy et al 2011). No data on sediments were collected in the present study, but it could be logically assumed that the greater intensity of precipitations in winter (Dias et al 2002) might cause a larger input of terrigenous sediments on the shore. This input might have caused favourable conditions for the development of larger covers of encrusting S. alveolata in winter than in summer.…”
Section: Discussionmentioning
confidence: 69%
“…trampling) disturbances, which can damage the existing bioconstructions and reduce the density of new recruits (Dubois et al 2002(Dubois et al , 2006. On the studied shore, mechanical impacts from waves and trampling have clear seasonal patterns related to the occurrence of extreme storms, mostly in winter (Dias et al 2002) and human frequentation of the shore, which is particularly intense in summer (Araújo et al 2009). As extreme waves could directly cause seasonal differences in the abundance of S. alveolata that are opposite to the present patterns and trampling might drastically affect intertidal assemblages on emergent rock rather than in rock pools, both mechanisms are unlikely to provide convincing explanations to our findings.…”
Section: Discussionmentioning
confidence: 99%
“…1c): two shores at the open coast (out of both rías), two shores at the outer part of both rías and two shores at the inner part of the Ría de Vigo showing salinity values similar to those in fully marine environments. The open shore sites are exposed to wave height from NW of about 3 m, with maximum values of around 7 m from SW during storms (Dias et al 2002). In the outer part of the ría, swell is normally from NW and wave height decreased from 1.6 m in the outer part of the ria to 0.6 m in the inner part of the ría (Bernabeu et al 2012).…”
Section: Quantitative Sampling For Comparisons Among Shores With Diffmentioning
confidence: 99%