Dr Olivia Roth, Curriculum vitae

* Presented at the VI International Wadden Sea Symposium (Biologische Anstalt Helgoland, Wattenmeerstation Sylt, D-2282 List, FRG, 1--4 November 1988} 9 Biologische Anstalt Helgoland, Hamburg

Harald Asmus, Ragnhild Asmus AWI Wadden Sea Station Sylt

Sylt Rømø Den-mar k Lister Ley Høyer dyb Rømø dyb Pander Tief German y Lister Tief What are stabilising frame conditions Habitat diversity stabilises food webs by increasing species diversity and thus number of food resources for higher trophic levels

Eutrophication of the Dutch Wadden Sea: External nutrient

* Presented at the VI International Wadden Sea Symposium (Biologische Anstalt Helgoland, Wattenmeerstation Sylt, D-2282 List, FRG, 1-4 November 1988) + Publication No 18 of the project "Ecological Research of the North Sea and Wadden Sea" (EON) 9 Biologische Anstalt Helgoland, Hamburg

Maritime Administration Perspective Nico Nolte, Federal

Symposium Underwater Noise, -For the calving ground „Sylt Outer Riff“ not more than 1 of the area may be disturbed Management strategy–Reducingthenoiseinput

Changes of the tidal water levels at the German North Sea coast

* Presented at the VI International Wadden Sea Symposium (Biologische Anstalt Helgoland, Wattenmeerstation Sylt, D-2282 List, FRG, 1---4 November 1988} 9 Biologische Anstalt Helgoland, Hamburg

ECSA Newsletter, 2008-11-21 (No

ECSA Symposium 46 "CHANGE OF COASTAL SYSTEM FUNCTIONING", 3-6 May 2010, Sylt, Germany 2011 Events: ECSA Symposium 49 "ESTUARIES & COASTS: TWO HEMISPHERES, ONE WORLD", April 2011,

Distribution, patchiness, and popula- tion densities of

were presented at the 6th International Wadden Sea Symposium, held at Sylt in November 1988 and subsequently published in the proceedings (De Wolf, 1989) However, this was not the end but the beginning of the story Piet became more and more intrigued by Pleurobrachia and its life cycle: the unexpected and unexplained population explosions

OSL en C14 dateringen van de kerk en het grafveld van de

Symposium Series, Volume 8, 2011 _____ 4 - sediment for transgressive dunes or aeolian sand-sheets Indeed, the formation of a transgressive dune at the Świna barrier and the deposition of aeolian cover sands in Sylt were dated to ~1500-1600 AD indicating enhanced aeolian activity during the main phase of the LIA Figure 1