<p>An influence at one trophic level can result in dynamic impacts also on other components of a food web. These dynamics are known as trophic cascades, and can be both top-down and bottom-up. After a near-collapse of the Baltic cod <i>Gadus morhua</i> stock in the 1980s, its main prey sprat <i>Sprattus sprattus</i> increased dramatically. The main food of sprat, marine copepods, decreased during the same time period, likely a combined effect of increased predation pressure from sprat and decreasing salinities. This shortage of food for sprat resulted in decreasing quality of sprat as a food source for common guillemots <i>Uria aalge</i>. However, a recent increase in fishing for sprat has again resulted in better feeding conditions for guillemots.</p><p>Human impacts on this simple food web can be complex. In the early 20th century, marine mammals were abundant and nutrient levels were low in the Baltic Sea. This thesis illustrate that this situation corresponded to lower fish biomass. A reduction of seals early in the century led to reduced top-down control, which resulted in increasing fish stocks. Later, in the 1950s, the largest inflow of salt water during the century mobilized accumulated phosphorus from the deep sediments, which stimulated nitrogen fixation. Combined with increasing anthropogenic nutrient loads, this led to increased primary production and a rapid change from an oligotrophic to a eutrophicated state. This change can be termed a regime shift, which also stimulated fish production. Subsequent over-fishing of cod likely caused a second regime shift, from a cod- to a clupeid- dominated state, which led to the described effects on the common guillemots.</p><p>Several factors affect the life-history of this long-lived seabird. Bycatches in gillnet fisheries is one factor directly affecting guillemot survival, and the proportion of bycatches increased during a period of increasing fishing effort. Surprisingly, avian cholera, a previously undocumented disease in common guillemots, was found at times to cause considerable adult mortality. Common guillemot life-history information can communicate the diversity of factors influencing marine ecosystems – hopefully this can increase our understanding of how complex even "simple" food webs are.</p>

An influence at one trophic level can result in dynamic impacts also on other components of a food web. These dynamics are known as trophic cascades, and can be both top-down and bottom-up. After a near-collapse of the Baltic cod Gadus morhua stock in the 1980s, its main prey sprat Sprattus sprattus increased dramatically. The main food of sprat, marine copepods, decreased during the same time period, likely a combined effect of increased predation pressure from sprat and decreasing salinities. This shortage of food for sprat resulted in decreasing quality of sprat as a food source for common guillemots Uria aalge. However, a recent increase in fishing for sprat has again resulted in better feeding conditions for guillemots. Human impacts on this simple food web can be complex. In the early 20th century, marine mammals were abundant and nutrient levels were low in the Baltic Sea. This thesis illustrate that this situation corresponded to lower fish biomass. A reduction of seals early in the century led to reduced top-down control, which resulted in increasing fish stocks. Later, in the 1950s, the largest inflow of salt water during the century mobilized accumulated phosphorus from the deep sediments, which stimulated nitrogen fixation. Combined with increasing anthropogenic nutrient loads, this led to increased primary production and a rapid change from an oligotrophic to a eutrophicated state. This change can be termed a regime shift, which also stimulated fish production. Subsequent over-fishing of cod likely caused a second regime shift, from a cod- to a clupeid- dominated state, which led to the described effects on the common guillemots. Several factors affect the life-history of this long-lived seabird. Bycatches in gillnet fisheries is one factor directly affecting guillemot survival, and the proportion of bycatches increased during a period of increasing fishing effort. Surprisingly, avian cholera, a previously undocumented disease in common guillemots, was found at times to cause considerable adult mortality. Common guillemot life-history information can communicate the diversity of factors influencing marine ecosystems – hopefully this can increase our understanding of how complex even "simple" food webs are.

Seagrasses constitute the basis for diverse and productive ecosystems worldwide. In East Africa, they provide important ecosystem services (e.g. fisheries) but are potentially threatened by increasing resource use and lack of enforced management regulations. The major aim of this PhD thesis was to investigate effects of anthropogenic distur-bances, primarily seaweed farming and coastal fishery, in East African seagrass beds. Seaweed farming, often depicted as a sustainable form of aquaculture, had short- and long-term effects on seagrass growth and abundance that cascaded up through the food web to the level of fishery catches. The coastal fishery, a major subsistence activity in the region, can by removing urchin predators indirectly increase densities of the sea urchin Tripneustes gratilla, which has overgrazed seagrasses in several areas. A study using simulated grazing showed that high magnitude leaf removal – typical of grazing urchins – affected seagrasses more than low magnitude removal, typical of fish grazing. Different responses in two co-occurring seagrass species furthermore indicate that high seagrass diversity in tropical seagrass beds could buffer overgrazing effects in the long run. Finally, a literature synthesis suggests that anthropogenic disturbances could drive shifts in seagrass ecosystems to an array of alternative regimes dominated by other or-ganisms (macroalgae, bivalves, burrowing shrimp, polychaetes, etc.). The formation of novel feedback mechanisms makes these regimes resilient to disturbances like seagrass recovery and transplantation projects. Overall, this suggests that resource use activities linked to seagrasses can have large-scale implications if the scale exceeds critical levels. This emphasizes the need for holistic and adaptive management at the seascape level, specifically involving improved techniques for seaweed farming and fisheries, protection of keystone species, and ecosystem-based management approaches.

Livestock production is one of the largest and fastest growing agricultural subsectors in the world, contributing almost 40 % of agricultural GDP. The present global trend of livestock intensification affects water demand, resulting in local alterations of hydrological features. This study quantifies water requirements for livestock production and links them to local changes in water-related ecosystem services (WRES). It examines the present situation in Uruguayan beef production as it undergoes an intensification process by analyzing three systems: traditional extensive production, mixed systems and intensive production.Mixed production systems are most water-effective in terms of water requirement. However, extensive production has the least negative long-term effects on the studied WRESs: soil productivity, erosion control and grass, crop and livestock production. Intensive systems contribute the largest negative impacts on soil productivity due to management practices, e.g. continuous cropping and fertilizer application (which is also costly). However, intensification also increases short-term positive effects on crop and livestock production. Mixed systems offer opportunities to increase livestock production, water use efficiency and mitigate soil degradation. However, a threshold value to avoid an undesirable regime shift in soil productivity remains to be determined.This framework developed herein, maps and quantifies local ecosystem effects associated with livestock production from a water perspective. It required simplifications and thus needs further improvements to be of practical use as a tool for best management practices of livestock production. Such tools can assist decision-makers in Uruguay on how to manage multiple ecosystem services in an agricultural landscape and enhance the provision of desired ES without degrading other key ecosystem processes, goods and services. For sustainable production of livestock in Uruguay, one should consider if the tradeoff between long-term negative impacts of intensification on regulating services is justifiable in the context of the short-term economic gains in provisioning services.

MSc (Zoology)) / Department of Zoology

La variabilité du contenu de chaleur hivernal de l'océan supérieur et ses mécanismes de causalité ont été étudiés en utilisant des observations et des produits de réanalyse dans le Pacifique Nord-Ouest. La relation entre la mousson d'hiver dans l'Asie de l'Est (EAWM) et l'Oscillation du Pacifique Nord (NPO) et leurs impacts sur la température de surface de la mer (SST) sont non stationnaires, avec un changement soudain en 1987/1988. L'EAWM et la NPO, qui étaient bien corrélées en 1973-1987, ne sont pratiquement plus corrélées en 1988-2002. Cette relation non stationnaire est liée au fort affaiblissement décennal de la haute pression Sibérienne après le changement de régime en 1988, ainsi qu'au changement concomitant du dipôle de la NPO positive. L'influence de l'EAWM et de la NPO sur la SST hivernale dans la région d'étude a significativement diminué après 1990. Le bilan de chaleur dans les 400 premiers mètres a été analysé à l'aide des sorties d'un modèle de la circulation océanique générale à haute résolution. Le taux de stockage de chaleur hivernal des échelles interannuelles à décennales est principalement déterminé par l'advection océanique plutôt que par le flux net de chaleur air-mer. Le rôle de l'advection de chaleur devient particulièrement important après le changement de régime en 1990, en association avec la réduction de la variabilité du flux de chaleur en surface causée par une faible variabilité de la SST. Le flux net de chaleur air-mer freine les anomalies thermiques créées par la dynamique océanique associée avec le déplacement méridien du front de l'Extension de l'Oyashio, qui est fortement corrélé avec les modes de téléconnexion de WP et PNA. / Winter upper-ocean heat content variability and its causal mechanisms are investigated using observational and reanalysis products in the western North Pacific. The relationship between the East Asian winter monsoon (EAWM) and the North Pacific Oscillation (NPO) and their impact on the sea surface temperature (SST) are nonstationary, with a sudden change at 1987/1988. During the 1973-87, the EAWM and NPO were significantly correlated to each other, but their correlation practically vanishes during the 1988-2002. This nonstationary relationship is related to the pronounced decadal weakening of the Siberian high after the 1988 regime shift as well as the concomitant positive NPO-like dipole change. The influence of EAWM and NPO to the winter SST in the study region is significantly decreased after the sudden change near-1990. The upper 400 m heat budget in the western North Pacific is analyzed using outputs from a high resolution ocean general circulation model. Winter heat storage rate on interannual to decadal time scales is mainly determined by oceanic heat advection rather than by net air-sea heat flux. The role of heat advection becomes particularly prominent after the 1990 regime shift in association with the reduced variability of surface heat flux caused by weakened SST variability. The net heat flux acts to dampen temperature anomalies caused by the ocean dynamics principally associated with the meridional shift of the Oyashio Extension front, which is significantly correlated with the West Pacific (WP) and Pacific-North America (PNA) teleconnection patterns.