The Helgoland Roads time series is one of the richest temporal marine data sets available. Running since 1962, it documents changes for phytoplankton, salinity, Secchi disc depths and macronutrients. Uniquely, the data have been carefully quality controlled and linked to relevant meta-data, and the pelagic time series is further augmented by zooplankton, intertidal macroalgae, macrozoobenthos and bacterioplankton data. Data analyses have shown changes in hydrography and biota around Helgoland. In the late 1970s, water inflows from the south-west to the German Bight increased with a corresponding increase in flushing rates. Salinity and annual mean temperature have also increased since 1962 and the latter by an average of 1.67°C. This has influenced seasonal phytoplankton growth causing significant shifts in diatom densities and the numbers of large diatoms (e. g. Coscinodiscus wailesii). Changes in zooplankton diversity have included the appearance of the ctenophore Mnemiopsis leidyi. The macroalgal community also showed an increase in green algal and a decrease in brown algal species after 1959. Over 30 benthic macrofaunal species have been newly recorded at Helgoland over the last 20 years, with a distinct shift towards southern species. These detailed data provide the basis for long-term analyses of changes on many trophic levels at Helgoland Roads.

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The paper briefly summarizes what is known about long-term changes (facts, causes, consequences) in the macrozoobenthos of intertidal and subtidal hardbottom communities around the island of Helgoland (German Bight, North Sea). There is increasing observational evidence that these communities (spectrum and abundances of species) are changing on a long-term temporal scale. The reasons are diverse and mainly anthropogenic. A shift in North Sea climate towards more oceanic conditions may be among the most important factors driving the recent changes in species spectrum. Many of the species which have been recorded as new to the Helgoland area during the past decade are southern (oceanic) species which may be considered as indicators of a warming trend.

Factors controlling the timing of reproduction in laboratory cultures of the polychaete Typosyllls prolifera. Typosyllis prolifera (Krohn) from Pore~ (Yugoslavia) has been cultured for 12 successive generations. The life cycle of the species in the laboratory is described briefly. During their life individuals reproduce several times (up to 15) by stolonization which, under constant laboratory conditions (LD 16:8, 20 °C), is cyclic and takes place about every 30 days. Based on the investigations of Durchon (1959) and Wissocq (1966), experiments on extirpation and transplantation of the proventriculus have been carried out. The results suggest that an endocrine system anatomically connected to the proventriculus is important in the control of reproduction. Most likely, the endogenous reproductive cycle of an individual is controlled by periodical changes of the activity of this system. During the period following stolonization, the endocrine system of the proventriculus, which at this time shows its maximal activity, inhibits sexual development and enables regeneration of the segments lost as stolon. A subsequent decrease of the hormonal activity induces sexual maturation and epitokous metamorphosis, thus leading to further stolonization. Exogenous factors influencing the timing of reproduction probably affect the endocrine function of the proventriculus. Short-day photoperiods (LD 10:14) and low temperatures (12 °C) given simultaneously (i.e. winter conditions) totally suppress reproduction. Under normally favourable conditions (LD 16:8, 20 °C),reproductive processes can be prevented by starving or amputation of caudal segments. In all these cases, however, stolonization can be induced by removing the proventriculus. Exogenous factors also play a decisive role in synchronizing reproductive events within the species population. Under field conditions reproduction shows a lunar periodicity. The endogenous reproductive cycles of cultured specimens can be synchronized by a periodical light regime simulating the change of the moon. EINLEITUNG