Transportation infrastructure is a major source of stormwater runoff that can alter hydrology and contribute significant loading of nutrients, sediment, and other pollutants to surface waters. These increased loads can contribute to impairment of streams in developed areas and ultimately to Lake Champlain. In this study we selected six watersheds that represent a range of road types (gravel and paved) and road densities (rural, suburban, and urban) present in Chittenden County, one of the most developed areas in Vermont. The location and density of road networks were characterized and quantified for each watershed using GIS analysis. Monitoring stations in each watershed were constructed and instrumented to measure discharge and water quality parameters continuously from spring through early winter. Storm event composite samples and monthly water chemistry grab samples were collected and analyzed for total nitrogen, total phosphorus, chloride, and total suspended sediments. Results from this study show that road type and road density are closely linked with the level of impairment in each watershed. Total phosphorus and total nitrogen from storm event composite samples and monthly grab samples significantly increased along a gradient of increasing road network density. Chloride concentrations increased several orders of magnitude along this same gradient. With the exception of Alder Brook where total suspended sediment (TSS) concentrations tended to be high, there were no significant differences in TSS concentrations between rural and developed watersheds. The elevated storm event TSS concentrations in the rural streams suggest that the unpaved roads in the rural watersheds contribute to stormwater runoff loads and that sediment control, at least in the developed watersheds, might be fairly effective. The overall results from this study show that local roads are a significant source of impairment for streams in the Chittenden County area. Most of these roads are municipal roads that are not under management of the Vermont Agency of Transportation. Thus, local actions will be necessary to reduce runoff and pollutant loading from these roads.

Constraining past episodes of climate change and glacial response is critical for understanding future impacts of climate change, especially in the high latitudes where warming is expected to be rapid and most of Earth's glaciers exist. Many studies of past glacier size utilize rare isotopes called cosmogenic nuclides to perform surface exposure dating. Since most areas of Earth's surface that were previously glaciated were covered by erosive ice, which stripped away pre-existing cosmogenic nuclides, surface exposure dating yields the timing of the most recent deglaciation. However, in some high latitude areas where glacial ice is cold-based and non-erosive (so-called 'ghost glaciers'), the assumptions of surface exposure dating are violated. Alternate approaches are required to constrain the complex histories of such landscapes. My doctoral dissertation focuses on both developing and employing alternative approaches to studying glacial history in the high latitudes, where glacial ice is non-erosive and dating rock surfaces with a single cosmogenic nuclide does not yield exposure ages. Here, I utilize optimized laboratory methods, paired analyses of two cosmogenic isotopes (10Be and 26Al), numerical models to assess possible exposure/burial histories, and Monte Carlo simulations to constrain uncertainties. To study the exposure and burial history of long-preserved landscapes in the Arctic, I investigate landscapes in two high-latitude locations: Thule, northwestern Greenland; and Cumberland Sound, southern Baffin Island, Canada. Bedrock surfaces, sampled on Baffin Island, exhibit evidence of long-lived subaerial weathering and have simple 10Be exposure ages up to 160,000 yr, despite being glaciated until ~10,000 yr. Simple exposure ages tend to increase with elevation, suggesting more effective erosion in the fjords and longer-term preservation of the uplands. Minimum limiting total histories calculated with 26Al/10Be range up to several million years, with periods of exposure representing ~20% of the total history, describing surfaces that have been alternately preserved beneath non-erosive glacial ice and weathered subaerially over many glacial/interglacial cycles. Boulders, sampled at both sites, have simple 10Be exposure ages up to 78,000 yr in Thule and 79,000 yr on Baffin Island, and yield multi-modal age distributions. Simple exposure ages of boulders tend to under-estimate bedrock ages in the cases of paired bedrock/boulder samples. Minimum limiting total histories calculated with 26Al/10Be range up to 700,000 yr in Thule and several million years on Baffin Island, with periods of exposure representing only a small portion of the total history. Forward numerical models suggest that boulders have been repeatedly reworked, likely experiencing partial or complete shielding during interglacial periods because of rotation and/or burial by till. The landscapes I assess here preserve histories of hundreds of thousands to millions of years, and represent a complex interplay of interglacial exposure, subglacial preservation beneath cold-based ice, periglacial processes, and subaerial weathering. Although such landscapes represent methodological challenges, they contain valuable information about long-term variations in glacial extent and climate.

Erosion, a surface process, can be quantified over long-term (assumed to be the natural erosion rate of the landscape) and contemporary (modern) timeframes. My research used the rare cosmogenic isotope 10Be in sand and cobbles collected from rivers in southeastern Brazil (Santa Catarina and Rio de Janeiro states) and southwestern China (Yunnan province) to quantify long-term, background rates of erosion and sediment supply. These measurements will also increase number of such measurements in tropical and subtropical climates. I assessed the relationship between landscape parameters (topographic and climatic) and background erosion rates in order to understand factors related to erosion. My data from so far unsampled states in Brazil shows that background erosion rates range between 13 and 90 m/Myr. I found that mean basin slope (R2=0.73) and mean annual precipitation (R2=0.57) are strongly correlated to erosion rates. Steep, escarpment-draining basins in Brazil erode faster than lower gradient basins draining the highlands. Comparing the isotopic concentration of river sand and cobbles, my data show that these grain sizes are sourced from different parts of the landscape. I compiled all published Brazilian cosmogenic 10Be data, and compared them to erosion rates from similar tectonic settings. While the erosion rates in Brazil are relatively low, they are similar to those in southeastern North America, but faster than rates measured on escarpments in southern Africa. In China, I tested the human effects on denudation by comparing long-term erosion rates derived from in-situ 10Be concentration and the modern sediment yield of 22 watersheds in Yunnan. Background erosion rates range between 17 and 386 m/Myr; long term sediment yields based on these erosion rates range from 79 to 893 tons km-2 yr-1. Modern sediment yields range from 90 to 2,879 tons km-2 yr-1 (data from Schmidt et al., 2011). In most watersheds, the modern sediment yield is 2-3X higher than long-term rates, likely the effect of a long history of land use in Yunnan. I found a statistically significant, positive relationship between erosion rates and both area (R2 = 0.60) and mean basin slope (R2 = 0.42). There is a negative but strong relationship between erosion rates and precipitation in my dataset (R2 = 0.60). I sampled some places where 10Be samples had been collected before to test the methodological assumption of time-invariant 10Be concentration. Concentrations generally agree on samples taken 6 months apart and in samples from the active channel and from floodplains, but not in samples collected a decade and centuries apart.

Rivers deliver significant macronutrients and sediments to lakes that can vary substantially throughout the year. These nutrient and sediment loadings, exacerbated by winter and spring runoff, impact aquatic ecosystem productivity and drive the formation of harmful algae blooms. The source, extent and magnitude of nutrient and sediment loading can vary drastically due to extreme weather events and hydrologic processes, such as snowmelt or high flow storm events, that dominate during a particular time period, making the temporal component (i.e., time over which the loading is estimated) critical for accurate forecasts. In this work, we developed a data-driven framework that leverages the temporal variability embedded in these complex hydrologic regimes to improve loading estimates. Identifying the "correct" time scale is an important first step for providing accurate estimates of seasonal nutrient and sediment loadings. We use water quality concentration and associated 15-minute discharge data from nine watersheds in Vermont's Lake Champlain Basin to test our proposed framework. Optimal time periods were selected using a hierarchical cluster analysis that uses the slope and intercept coefficients from individual load-discharge regressions to derive improved linear models. These optimized linear models were used to improve estimates of annual and "spring" loadings for total phosphorus, dissolved phosphorus, total nitrogen, and total suspended loads for each of the nine study watersheds. The optimized annual regression model performed ~20% better on average than traditional annual regression models in terms of Nash-Sutcliffe efficiency, and resulted in ~50% higher cumulative load estimates with the largest difference occurring in the "spring". In addition, the largest nutrient and sediment loadings occurred during the "spring" unit of time and were typically more than 40% of the total annual estimated load in a given year. The framework developed here is robust and may be used to analyze other units of time associated with hydrologic regimes of interest provided adequate water quality data exist. This, in turn, may be used to create more targeted and cost-effective management strategies for improved aquatic health in rivers and lakes.

Anthropogenic inputs of nutrients and sediment are a widespread problem in U.S. streams causing localized impairment and contributing to eutrophication of coastal habitats. Sediments and dissolved nutrients interact through diverse processes including ion exchange, sorption and biotic assimilation by particle-bound bacteria. This study examined the effects of sediment re-suspension on nutrient partitioning in lab microcosms using fine benthic matter collected from two Virginia Coastal Plain streams. Kimages Creek was recently restored following dam removal and was characterized by large deposits of legacy sediments. Courthouse Creek was characterized by sandy substrates typical of Coastal Plain streams. Sediment characteristics differed between the two sites and were influenced by discharge. Net nutrient release rates were similar between streams though reactivity of Courthouse Creek sediments was greater than that of Kimages Creek. Equilibrium Phosphate Concentrations calculated for each site show that fine sediments at Kimages Creek have resulted in higher phosphorus retention potential.

Native oysters have been promoted as a means to improve water quality in Chesapeake Bay. This project added important insights into the potential of oyster aquaculture to process and remove nutrients from Bay waters. Results clarified that nutrient removal of nitrogen (N), phosphorous (P), and carbon (C) through harvest of cultivated oyster biomass can be quantified and modeled with high levels of statistical confidence. A simple, yet accurate, method is now available for estimating the amount of nutrients removed via harvesting aquacultured oysters. Based on model estimates, 106 harvest sized oysters (76 mm TL) remove 132 kg TN, 19 kg TP, and 3,823 kg TC. Previous work suggested that potentially substantial quantities of N may be removed through enhancement of the coupled nitrification-denitrification pathway in sediments as a result of oyster biodeposition. Using 15N and N2/Ar methods to measure N2 production in sediments, encompassing direct denitrification (DNF), coupled nitrification- denitrification, and anaerobic ammonium oxidation (anammox) pathways, at two oyster aquaculture sites and two reference sites (no aquaculture), we found that oyster biodeposition did not accelerate sediment N removal. We estimate sediment N removal rates via N2 production at an oyster cultivation site producing 5 x 105 oysters (1750 m2) to range from 0.49-12.60 kg N yr-1, compared to 2.27-16.72 kg N yr-1 at a reference site of the same area; making the contribution of oyster cultivation to N removal via sediment N2 production inconsequential as a policy initiative for Chesapeake Bay eutrophication mitigation. Molecular approaches and direct abundance measures have improved our understanding of the sediment microbial community response to oyster biodeposition. Overall, sediments impacted by oyster biodeposition had a significantly different denitrifying community composition than sediments a few meters away or at the non-aquaculture reference sites. Bacterial abundance in sediments was determined by site rather than by oyster biodeposition. No apparent effects of oyster biodeposition were evident in nitrifying bacterial abundance patterns at either site, indicating that oyster biodeposition does not enhance coupled nitrification-denitrification by increasing the abundance of nitrifiers in sediments.

Thorium-230 and protactinium-231 have been widely used as proxies of oceanic processes in both modern and past marine environment. Their application as such proxies is, however, limited by sparse data from the modern ocean with which to characterize their distribution and behavior. This thesis aims to provide such data and to assess their uses as oceanic proxies for ocean circulation, sediment dissolution, and modern dust input. Twelve profiles of dissolved ²³⁰Th, ²³¹Pa and ²³²Th obtained on a meridional GEOTRACES section in the Southwest Atlantic confirm the expected transport and fractionation of ²³¹Pa from ²³⁰Th by deep ocean circulation out of the modern Atlantic. There is however neither a water mass dependence nor progressive change as water masses age, which challenges the use of sedimentary ²³¹Pa/²³⁰Th to assess past flow in the South Atlantic. Decreases of ²³⁰Th and ²³¹Pa observed in near-bottom water indicate enhanced sea-floor removal in regions where nepheloid layers are present. In a second study of sedimentary nuclides concentration, high-resolution ²³⁰Th_xs profiles from sediment in Southeast Atlantic exhibit increasing ²³⁰Thxs concentrations from core-top to a depth of ∼3 cm followed by relatively constant values at greater depth, suggestive of sediment dissolution in the upper sediment core. This observation suggests the use of ²³⁰Thxs to quantify sediment dissolution. Combined with sediment composition measurements, ²³⁰Th_xs also provides an assessment of which constituents are dissolving from the sediment. (²³¹Pa/²³⁰Th)_xs ratios do not appear to be affected by sediment dissolution. A third study, in the tropical Atlantic Ocean, combines water-column measurements of ²³⁰Th, ²³²Th with coeval aerosol measurements, and allows assessment and improvement of the use of ²³²Th to quantify dust input to the surface ocean. ²³²Th-derived dust flux increases from 0.43 g/m²/yr at low latitude in the South Atlantic to 10.70 g/m²/yr at higher latitude in the North Atlantic, and broadly agree with a model of dust input. The data presented in this thesis have expanded the dataset of ²³⁰Th, ²³²Th and ²³¹Pa in the Atlantic Ocean, and provide an insight into future uses of these nuclides as oceanic proxies.

L'altération chimique de la croûte terrestre fournit à l'ensemble des cycles bio-géochimiques de la surface les éléments essentiels à leur fonctionnement. L'érosion de grands orogènes, comme la chaîne Himalayenne s'accompagne de flux d'érosion et d'altération significatifs, susceptibles d'avoir un impact à l'échelle globale. L'objectif de cette thèse est de comprendre comment les processus physiques et chimiques façonnent le signal sédimentaire afin de quantifier l'érosion et l'altération actuelle ainsi que leur variations passées. L'étude détaillée de la dynamique du transport sédimentaire et des caractéristiques physiques et géochimiques des sédiments dans le bassin du Gange montre qu'actuellement environ 10 % du flux sédimentaire érodé en Himalaya est séquestré dans la plaine alluviale du Gange. L'utilisation des isotopes cosmogéniques (10Be) dans les sédiments de rivières montrent des taux d'érosions stables entre 1.3 et 1.4 mm par an pour l'ensemble de la chaîne drainée par le Gange. De plus, le transfert de sédiments dans la plaine s'accompagne d'un appauvrissement en éléments mobiles marquant l'altération chimique de ceux-ci. Cette altération a été quantifié et suggère que la plaine du Gange joue un role dominant dans l'altération des sédiments Himalayens. Les échanges cationiques lors du passage des sédiments au domaine marin restent limités dans le cas du système Himalayen et ne permettent d'augmenter le bilan de stockage de carbone à long terme que de 20 % environ. Enfin, l'enregistrement de la Baie du Bengale, qui couvre les produits issus de l'érosion Himalayenne sur les derniers 20 000 ans, montre que les sédiments exportés au Dernier Maximum Glaciaire (DMG) étaient significativement moins altérés qu'à l'actuel. Le système Himalayen n'est donc pas tamponné vis-à-vis des forages climatiques à haute fréquence du Quaternaire et les taux d'altération actuels ne peuvent très extrapolés dans le passé. / Chemical weathering of the earth crust supplies the essential elements for numerous biogeochemical cycles. Physical erosion of large orogens, such as the Himalayan range, is accompanied by significant weathering fluxes possibly affecting the global environment. The objective of this PhD is to understand how surface processes affect river sediment properties in order to asses current erosion and weathering rates but also to decipher their past variations. To answer this question we studied the transport dynamics, the physical and the geochemical characteristics of the sediments in the Ganga basin. This study suggests that about 10 % of the flux eroded in the Himalayas is currently stored in the Ganga floodplain. Cosmogenic isotopes (10Be) measured in river sediments show stable erosion rates between 1.3 and 1.4 mm/yr for the entire Himalayan range drained by the Ganga. Furthermore, we show that River sediments are progressively depleted in the most mobile elements, as weathering proceeds during transfer in the floodplain. By comparing this flux to the weathering flux of the Himalayan range, we show that floodplain weathering is predominant in weathering Himalayan sediments. Cation exchange occurring when Ganga and Brahmaputra (G&B) sediments enter the marine environment are limited and enhances the long term carbon storage, linked to silicate weathering by only ca. 20 %. Finally, the Bay of Bengal sedimentary record, which documents the last 20 000 years of Himalayan erosion shows that the sediments exported during the last glacial maximum (LGM) were significantly less weathered compared to the sediments currently exported. The Himalayan system is thus not buffered towards the high frequency climate forcing changes of the Quaternary and modern weathering rates cannot easily be extrapolated over the past.

L'évolution sédimentaire des milieux lagunaires est un phénomène complexe faisant intervenir à la fois des processus intenses sur le court terme (crues, tempêtes) et des processus plus lents sur le long terme (variations du niveau marin moyen, changements climatiques). Si les mécanismes généraux de ces phénomènes sont bien connus, leur variabilité spatiale et temporelle les rends difficiles à estimer au niveau local. La grande diversité des milieux lagunaires et l'influence des actions anthropiques rendent plus hasardeuse encore cette estimation. Dans cette étude, je me suis intéressé au cas du système lagunaire méditerranéen des « étangs Palavasiens, étang de l'Or, canal du Rhône à Sète » situé dans le Golfe du Lion (Sud de la France). L'utilisation d'une approche pluridisciplinaire a permis d'évaluer la dynamique sédimentaire sur des échelles de temps multiples. Sur les deux derniers siècles, le comblement du système lagunaire a pu être estimé à la vitesse moyenne de 1,3 mm.an-1 à travers l'utilisation conjointe de données géographiques historiques et d'analyses géochronologiques (210Pb, 137Cs). Une perte de surface imputable pour moitié aux aménagements anthropiques est également mise en avant au cours du XXème siècle. Une campagne de mesures haute fréquence de la dynamique hydro-sédimentaire a été menée à court-terme (2 ans). Elle a permis de déterminer l'influence des conditions de forçages physiques sur les processus internes (érosion, remise en suspension, dépôt). Les seuils caractéristiques tels que la tension critique d'érosion ont pu être estimés et reliés aux conditions météorologiques. Le bilan net sur les stations suivies durant cette période montre une perte de sédiment. Ce bilan opposé aux estimations historiques sur les mêmes secteurs est probablement en lien avec les conditions d'apports réduites durant la période investiguée. L'adaptation d'un modèle numérique sur la zone d'étude a été entreprise afin de préciser cette dynamique sur une plus large échelle spatiale et temporelle. / The sedimentary evolution of coastal lagoons is a complex phenomenon involving both short term extreme processes (floods, storms) and long term processes (mean sea level variations, climate change). If general mechanisms of these phenomena are well known, their spatial and temporal variability makes them difficult to assess at the local scale. The diversity of lagoonal environments and human influence makes this even more risky. I have focussed this study on the case of a Mediterranean lagoon system : “Palavasian lagoons, Or lagoon, and Rhône-Sète waterway” which is located in the Gulf of Lion (South of France). A multidisciplinary approach was used to assess sediment dynamics on multiple time scales. An average filling rate of 1.3 mm.year-1 over the two last centuries was assessed using a both historical maps and geochronology (210Pb, 137Cs). An area loss due for half to anthropogenic impacts was also highlighted in the twentieth century. A short term (2 years) and high frequency monitoring of in situ hydro-sedimentary dynamics was performed to determine the influence of physical forcing over internal processes (erosion, resuspension, deposition). The main characteristics thresholds were estimated and related to weather conditions. The observed net balance during this monitoring shows a loss of sediment. This assessment, opposite of historical trends, is probably related to the conditions of reduced river contribution. The implementation of a numerical model is going on in order to explain the dynamics on a larger spatial and temporal scales.

La colonisation médiévale scandinave au Groenland (986 – 1450 AD) et la reconquête agricole récente de la région sud-groenlandaise, favorisée par le réchauffement climatique en cours, constituent un modèle de référence particulièrement adapté à l’étude des relations entre une communauté humaine et son environnement. Dans cette perspective, une étude sédimentologique multiparamètre a été réalisée sur la séquence sédimentaire du lac d’Igaliku (N61°00’22”, W45°26’28”), situé au cœur de la principale implantation médiévale et du secteur agro-pastoral contemporain. Quatre mètres de sédiments, couvrant la totalité de l’évolution holocène du lac (~10000 ans), ont été étudiés à haute résolution temporelle. L’analyse comprend une caractérisation physico-chimique (densité, susceptibilité magnétique, diagraphie XRF, imagerie rayon-X, granulométrie laser, dosages carbone, azote et souffre, ICP-AES, isotopie δ13C et δ15N de la matière organique) et biologique (pollen, microfossiles non polliniques, diatomées) du sédiment. Vingt-huit datations radiocarbones, ainsi que la mesure l’activité du 210Pb et du 137Cs, permettent d’interpréter le signal sédimentaire dans un cadre chronologique très précis et de reconstruire l’évolution postglaciaire du lac et de son bassin versant, soumis aux contraintes glacio-isostatiques, aux forçages climatiques et aux impacts anthropiques. La première phase d’évolution du système lacustre est principalement sous contrôle isostatique avec une transition rapide d’un environnement marin pro-glaciaire vers un environnement lacustre après émersion du bassin, il y a 9500 ans. Par la suite, la séquence témoigne de l’évolution paléoclimatique de la région. Les paramètres limnologiques et terrestres suggèrent un réchauffement précoce, probablement interrompu par une période froide, sèche et venteuse entre 8600 et 8100 ans cal BP. Un second événement sec et venteux, de 5300 à 4800 ans cal BP, précède la transition néoglaciaire, qui se caractérise, à Igaliku, par une évolution vers un climat plus humide et peut-être plus froid à partir de 4800 cal BP, provoquant une mutation majeure des conditions écologiques terrestres et aquatiques. La diminution des flux de grains de pollen indique un refroidissement notable à partir de 3000 cal BP. Vers l’an 1000, suite à l’arrivée des colons scandinaves, le système lacustre passe sous un contrôle anthropique dominant. Le défrichement et l’introduction d’herbivores domestiques dans le bassin versant du lac produisent un doublement du taux d’érosion des sols (de 4 mm/siècle à 8 mm/siècle vers 1200 AD) et une modification de la qualité des influx organiques. Pour autant, les assemblages de diatomées indiquent que l’écologie du lac n’a été que faiblement affectée par l’agriculture médiévale. A partir de 1325 AD et jusqu’à la fin de la colonie scandinave, vers la moitié du XVe siècle, la végétation présente des signes de résilience et l’érosion des sols régresse. Cette déprise agro-pastorale, probablement en relation avec les prémices du Petit Âge Glaciaire, est en phase avec une importante mutation des pratiques de subsistance attestée par l’archéologie. Le retour du pastoralisme au début du XXe siècle marque une reprise des processus d’érosion, similaires, en intensité, à ceux engendrés par les colons scandinaves. En revanche, l’intensification et la modernisation des pratiques agricoles dans les années 1980 est responsable d’une érosion des sols spectaculaire (~21 mm/siècle) et d’une mutation de l’écosystème lacustre (eutrophisation) sans précédent depuis la formation du lac, il y a 9500 ans. Les effets combinés de l’agriculture et du réchauffement climatique en cours (amorcé dans les années 1920 à Igaliku) aura des conséquences environnementales difficiles à prévoir pour l’avenir de la région / The medieval Norse colonization of Greenland (986-1450 AD) and the subsequent reestablishment of agriculture in south Greenland, aided by recent climate warming, constitute a conceptual model that is particularly well adapted to understanding the relations between a community and its environment. In this perspective, a multi-parameter sedimentological study was undertaken on the sedimentary sequence of Lake Igaliku (N61°00’22”, W45°26’28”), situated in the heart of the medieval and current agricultural sector. The 4 m long sequence, covering the entire Holocene evolution of the lake (~10 000 years), was studied at high temporal resolution. The analyses included the physico-chemical characterization of the sediments (density, magnetic susceptibility, XRF, X-ray imaging, grain size, carbon, nitrogen, and sulphur content, ICP-AES, δ13C and δ15N isotopic ratios) as well as the biological components of the sediment (pollen, non-pollen palynomorphs, diatoms). 28 radiocarbon dates as well as 210Pb and 137Cs measurements created a precise temporal framework with which to reconstruct the postglacial evolution of the lake and its catchment in terms of isostatic constraints, climatic forcing and anthropogenic impacts. The first phase of basin evolution is primarily controlled by isostasy, with the rapid transition from glaciomarine conditions to a freshwater lake as the basin emerged from the fjord 9500 yr BP. Afterwards, the sedimentary sequence records the paleoclimatic evolution of the region. Paleolimnological and terrestrial proxies suggest an early warm phase likely interrupted by a cold, windy, dry period between 8600 yr BP and 8100 yr BP. A second dry, windy period between 5300 yr BP and 4800 yr BP predated the transition to neoglacial cooling, which is characterised at Igaliku by a switch to humid and perhaps cooler conditions after 4800 BP, and which caused a major shift in both aquatic and terrestrial ecology. Approximately 1000 AD, after the arrival of Norse settlers, the lacustrine system became anthropogenically dominated. Land clearing and domestic herbivores introduction in the lake catchment doubled the rate of soil erosion (from 4 mm century-1 to 8 mm century-1 by 1200 AD) and caused a major modification of the organic carbon influx. On the other hand, diatom assemblages demonstrate that the lake ecology was not strongly impacted by medieval agriculture at this site. After 1325 AD, until the end of the Norse tenure in the mid-15th century, terrestrial vegetation showed signs of rebound and soil erosion decreased. This agricultural diminishment, probably in relation to the beginning of the Little Ice Age, is consistent with an important change in subsistence patterns evidenced by archaeology in this region. The reestablishment of agriculture at the beginning of the 20th century marks the reinvigoration of erosional processes that are similar in intensity to that of the Norse settlement. On the other hand, the intensification and modernization of farming practices during the 1980s is responsible for marked soil erosion (21 mm century-1) and a shift in lake ecology (eutrophication) that is unprecedented in the 9500 yr history of the lake. The combined effects of agriculture and climate warming already underway (initiated in the 1920s at Igaliku) will have large environmental consequences for the future of this region