scheldt estuary
Recently Published Documents


TOTAL DOCUMENTS

243
(FIVE YEARS 6)

H-INDEX

47
(FIVE YEARS 0)



2021 ◽  
Author(s):  
Dante M. L. Horemans ◽  
Yoeri M. Dijkstra ◽  
Michèle Tackx ◽  
Patrick Meire ◽  
Tom J. S. Cox


2021 ◽  
Author(s):  
Dante M. L. Horemans ◽  
Yoeri M. Dijkstra ◽  
Michèle Tackx ◽  
Patrick Meire ◽  
Tom J. S. Cox

Abstract. Estuaries often show regions in which Chlorophyll-a (Chl-a) accumulates. The location and magnitude corresponding to such accumulation result from a complex interplay between processes such as river flushing, salinity, nutrients, phytoplankton grazing, and the light climate in the water column. Of particular interest is the long-term evolution of the estuary-scale Chl-a distribution in the Scheldt estuary (Belgium/Netherlands) in spring. From 2004–2007, we observed a limited spring-bloom in the brackish region. This bloom intensified in 2008–2014 and disappeared after 2015. This long-term evolution in Chl-a has been linked to simultaneous long-term trends in the suspended particulate matter (SPM) distribution and the improvement of the water quality, which affects grazing of Chl-a by zooplankton. However, this hypothesis has not been systematically investigated. In this paper, we apply two approaches to test this hypothesis. In the first approach, we analyze long-term in situ observations covering the full estuary. These observations include the SPM concentration, zooplankton abundance, and other variables affecting the Chl-a concentration, and show a long-term estuary-scale evolution in not only the SPM distribution but also in zooplankton abundance, freshwater discharge, and maximum photosynthetic rate. In the second approach, we apply a model approach supported by these observations to determine which of the changed conditions may explain the observed change in Chl-a. Our results suggest that a change in SPM alone cannot explain the Chl-a observations. Instead, mortality rate and grazing by zooplankton mainly explains the long-term estuary-scale evolution of Chl-a in spring. Our results highlight that insight into the zooplankton dynamics is essential to understand the phytoplankton (cf. Chl-a) dynamics in the Scheldt estuary.





2021 ◽  
Vol 757 ◽  
pp. 143827
Author(s):  
Camille Gaulier ◽  
Chunyang Zhou ◽  
Yue Gao ◽  
Wei Guo ◽  
Marek Reichstädter ◽  
...  


2020 ◽  
Vol 245 ◽  
pp. 106967 ◽  
Author(s):  
Liesbeth De Neve ◽  
Gunther Van Ryckegem ◽  
Joost Vanoverbeke ◽  
Frank Van de Meutter ◽  
Alexander Van Braeckel ◽  
...  


2020 ◽  
Vol 530-531 ◽  
pp. 151437
Author(s):  
Jan Soors ◽  
Jan Breine ◽  
Cédric d'Udekem d'Acoz ◽  
Ericia Van den Bergh ◽  
Frank Van de Meutter ◽  
...  


ZooKeys ◽  
2020 ◽  
Vol 947 ◽  
pp. 143-155
Author(s):  
Tanja Milotic ◽  
Peter Desmet ◽  
Anny Anselin ◽  
Luc De Bruyn ◽  
Nico De Regge ◽  
...  

In this data paper three datasets are described containing GPS tracking and acceleration data of Western marsh harriers (Circus aeruginosus) breeding in Belgium and the Netherlands. The Western marsh harrier is included as a threatened bird species in Annex I of the European Bird Directive due to the steep decline in population densities. In order to collect data of habitat use and migration behaviour, Western marsh harriers were equipped with light-weight solar powered GPS trackers developed by the Institute for Biodiversity and Ecosystem Dynamics (IBED) at the University of Amsterdam (University of Amsterdam Bird Tracking System, UvA-BiTS). These trackers automatically collect and store data on the bird’s activity and 3D position in time and transmit these data to ground stations. The datasets were collected by the Research Institute for Nature and Forest (INBO) and the Dutch Montagu’s Harrier Foundation. Tracked Western marsh harriers were breeding in the northeast of the Dutch province of Groningen and on the opposite side of the river Ems in Germany (H_GRONINGEN), in the region of Waterland-Oudeman near the Belgian-Dutch border (MH_WATERLAND), and at the left bank of the Scheldt estuary, close to the Belgian-Dutch border and north of the city of Antwerp (MH_ANTWERPEN). Most individuals remained within 10 km from their nesting sites during the breeding season and wintered in West Africa. H_GRONINGEN contains 987,493 GPS fixes and 3,853,859 acceleration records of four individuals since 2012. MH_WATERLAND contains 377,910 GPS fixes of seven individuals. Sampling in this region began in 2013. Three more Western marsh harriers were tagged in the Scheldt estuary near Antwerp more recently in 2018 (one individual) and 2019 (two individuals) for the MH_ANTWERPEN study, which contains 47,917 GPS fixes and 227,746 acceleration records. The three Western marsh harrier datasets were published as separate studies in Movebank (https://www.movebank.org) and archived as data packages in Zenodo (https://www.zenodo.org) to ensure long-term preservation and versioning of the data.



2020 ◽  
Vol 146 (7) ◽  
pp. 05020004
Author(s):  
Y. Plancke ◽  
J. Stark ◽  
D. Meire ◽  
M. Schrijver


Sign in / Sign up

Export Citation Format

Share Document