An investigation of geological and geochemical characteristics of late-Quaternay sediments in the Georgian Bay Region, Southern Ontario

Core samples of postglacial sediments and sediment surface samples from Shepherd Lake on the Bruce Peninsula, Harts Lake on the Canadian Shield, and two cores from Georgian Bay (core P-l in the western deep part and core P-7 in the eastern shallow part) have been analyzed for pH, grain size distribution, water content, bulk density, loss on ignition at 4500C and 11000 C, major oxides (Si02 ,A1203,!FeO,MgO,CaO, Na20,K20,Ti02 ,MnO and P205) and trace elements (Ba,Zr,Sr,y,S, Zn,Cu,Ni,Ce and Rb). The sediment in Georgian Bay are generally fine grained (fine silt to very fine silty clay) and the grain size decreases from the Canadian Shield (core p-7) towards the Bruce Peninsula (core P-l) along the assumed direction of sediment transport. This trend coincides with a decrease in sorting coefficient and an increase in roundness. Other physical characteristics, such as water content, bulk density and loss on ignition are positively correlated with the composition of sediments and their compaction, as well as with the energy of the depositional environment. Analyses of sediment surface samples from Shepherd Lake and Harts Lake indicate the influence of bedrock and surficial deposits in the watershed on pH condition that is also influenced by the organic matter content and probably I ! I man's activities. Organic matter content increases significantly in the surface sediment in these small lakes as a result of either natural eutrophication or anthropogenic organic loading. The extremely high organic matter content in Shepherd Lake sediment indicates rapid natural eutrophication in this closed basin and high biological productivity during postglacial time, probably due to high nutrient levels and shallow depth. The chemical composition of the Canadian Shield bedrock is positively correlated with the chemical characteristics of predominantly inorganic lake sediments that were derived from the Shield rocks by glacial abrasion and by postglacial weathering and erosion of both bedrock and surficial deposits. High correlation coefficients were found between organic matter in lake sediments and major oxides (Si02,AI203,.~FeO, MgO,CaO,K20 and MnO) , as well as some trace elements (Ba,Y, S,Zn,Cu,Ni and Rb). The chemical composition of sediments in Harts Lake and core P-7 in Georgian Bay on the Canadian Shield differs from the chemistry of sediments in Shepherd Lake and core P-l in Georgian Bay on the Bruce Peninsula. The difference between cores P-l and P-7 is indicated by values of Si02 , AI203 ,:LFeo,Mgo,CaO,Ba,Zr,Sr,y and S, and also by the organic matter content. This study indicates that the processes of sediment transport, depositional environment, weathering of the rocks and surficial deposits in the watershed, as well as chemical composition of source rocks all affect the chemical characteristics of lake sediments. The stratigraphic changes and variations in lake sediment chemistry with regard to major oxides, trace elements, and organic matter content are probably related to the history of glacial and postglacial lake stages of the Georgian Bay Region and, therefore, the geochemical data can make a useful contribution to a better understanding of the Late-Quaternary history of the Great Lakes.

Palynology of late-glacial and postglacial sediments in Georgian Bay, Ontario, Canada, as related to the Great Lakes history /

This investigation comprises three parts: (1) the source, mechanism of transport, and distribution of pollen, spores and other palynomorphs in Georgian Bay bottom sediments and a comparison of these data with the contemporary vegetation, (2) the relative significance of fluvial transportation of pollen and spores, and (3) the late- and postglacial history of vegetational and climatic changes in the Georgicin Bay region. Modem pollen and spore assemblages in Georgian Bay do reflect the surrovinding vegetation when preservation and pollen production by the different species are considered and accounted for. Relative pollen percentage and concentration isopoll patterns indicate that rivers contribute large quantities of pollen and spores to Georgian Bay. This is further substantiated by large amounts of pollen and spores which were caught in traps in the Moon, Muskoka, and Nottawasaga Rivers which flow into Georgian Bay. The majority of pollen and spores caught in these traps were washed into the rivers by surface water runoff and so reflect the vegetation of the watershed in a regional sense. In a 12.9 metre long sediment core from northeastern Georgian Bay the relative percentage and absolute pollen concentrations allow correlation of Georgian Bay Lake phases with climatic and forest history. Four distinct pollen zones are distinguished: zone GB IV which is the oldest, reflects the succession from open spruce woodland to boreal forest; zone GB III represents a period of pine-mixed hardwoods forests from about 10,000 to 7,500 years ago. A pine-maplehemlock association dominated in zone GB II, although during the culmination of postglacial warming about 4,000 to 5,000 years ago the Georgian Bay forests had a more deciduous character. Zone GB I clearly shows European man's disturbance of the forest by logging activities.

Tourist travel via Grand Trunk Railway System : and connections, including Niagara Falls and Gorge, the Highlands of Ontario, comprising Georgian Bay, Muskoka Lakes ; St. Lawrence River, Montreal, Quebec, the Saguenay River, the Rangeley Lakes, White Mountains, and the Atlantic Sea-Coast /

Previous editions of this work have appeared under the title: Gateways of tourist travel.

Flyer for the Georgian Bay, Ontario Steam Show, 1983

Flyer for the Georgian Bay, Ontario Steam Show, 1983.

Petrography, Petrochemistry and petrogenesis of Huronian volcanic rocks of the Elliot Lake region, Ontario

In the Elliot lake region of northern Ontario, Yolcanlc lava piles represent the lowermost units of the Huronian SUpergroup. These rocks general1y trend east-west and belong to the Elliot lake Group. They are s1tuated on the north and south limbs or the QuIrke lake Syncline. The volcanIc rocks of this study contain a secondary minerai assemblage consisting of actinolite, biotite, chlorIte, eptdote/cllnozoislte tttanomagnettte and calcite characteristic of greenschist metamorphism. Compilation of data suggests that metamorphism of the volcanic rocks proceeded between 325- and 425-C and between 2.4 and 4.7 kb. Geochemtcally these lavas represent tholeiitic and calc-alkaline assemblages. The tholeiites are character1sttcally enriched tn Fe and Tt and consist mainly of basalts, basaltic andesites and andesites. These rocks are believed to have formed by the partIal melting of a peridottte source at low P-T. In contrast, the calc-alkaline rocks are depleted in Fe and TI, but show a signIficant enrichment In 51 and Zr; andesIte Is the major rock type for thIs assemblage. I·t Is postUlated that the calc-alkalIne sU1te of rocks was the result of eIther the partIal meltIng of abasaltic·magma at shallow depth, or the melttng of s1al1c crustal materIal due to the added we1ght of tholeiitIc material on an unstable crust and to downwarplng processes Inttlated by convection cells.

Distribution of barnacle epizoites of the crab Portunus pelagicus in the Moreton Bay region, eastern Australia

The parasites of some decapod crustaceans are known to cause sterilisation of their hosts, and can thus have an important impact on the population dynamics of infested species. Blue swimmer crabs (Portunus pelagicus) collected in three areas around Moreton Bay, Australia were examined for the presence of epizoic barnacles in their branchial chambers and on their carapace. Of the 952 crabs inspected 92% were infested with Octolasmis spp. The mean number of barnacles (predominantly Octolasmis warwickii) per carapace and gill chamber (mainly O. angulata) were 2.35 and 71.1, respectively. Barnacle infestation of gills was found to differ significantly by area, season and sex with the deeper offshore areas exhibiting the highest number of barnacles. The distribution within the hosts showed barnacles were more likely to be distributed in areas closer to the inhalant aperture. Highest abundances were found on the proximal surface of the hypobranchial side of gills 3, 4 and 5. Host moult stage and parasitism by Sacculina granifera were also found to affect the abundance of epizoic barnacles in some areas.

Wetland Tracker Data Collection Central Coast (Morro Bay Region)

The goal of this project was to gather information on wetland restoration projects in the Moro Bay, California, region. Data provided to the San Francisco Estuary Institute (SFEI) will be used to enhance a web-based, public access database, the Bay Area Wetland Project Tracker. Wetland Tracker provides information on the location, size, sponsors, habitats, contact persons, and status of included projects. Its website provides an interactive map of planned and completed wetland projects (http://www.wetlandtracker.org). (Document contains 4 pages)

A study of the intertidal sea anemones of the Monterey Bay region

This is a student paper done for a University of California Berkeley Zoology class. Since UCB didn't have its own marine lab at the time, it rented space at Hopkins Marine Station where this work was done. Cadet Hand earned his Ph.D. from Berkeley and went on to become Director of the Bodega Marine Laboratory. (PDF contains 36 pages)

Studies of the effects of industrial pollution in the lower Patapsco river area: 1. Curtis Bay Region 1941

Industrial effluents in the lower Patapsco area, which constitutes the navigable portion of the river and includes Baltimore Harbor, are many and include waste acid, distillery waters, tannery wastes and copper as (ferrous sulphate) from pigment and steel industries. (PDF contains 22 pages (2 on 1)

Pen and sunlight sketches of scenery reached by the Grand Trunk Railway system and connections with summer routes and fares to principal points : including Niagara Falls, Thousand Islands, Rapids of the St. Lawrence, Montreal, Quebec, Parry Sound, Georgian Bay, Muskoka Lakes, Adirondacks, Lake St. John, Mackinac Island, Midland District Lakes, the White Mountains, the Suquenay River, Rangeley Lakes and the sea-shore.--

At head of title: "Great tourist route of America".

Indigenous climate change adaption in the Port Philip Bay region : a longitudinal investigation into the physical and cultural transformation of the bay from an indigenous and landscape architectural perspective

Currently there is a dearth of research into Australian Indigenous knowledge and their understanding of climate change especially in regard to how it fits into their world view. Recent discussions by the National Climate Change Adaptation Research facility (NCCARF) have highlighted this deficiency but also the need to source relevant research projects that may address this knowledge and perspective, and enable the incorporation of Traditional ecological Knowledge into the planning climate change adaptions strategies in the Port Phillip Bay region thereby increasing their engagement in this discussion. Within this context, this paper examines the use and understanding of landscape, both urban and regional, surrounding Port Phillip Bay and the risks and opportunities climate change adaptation brings to the local Indigenous communities. It synthesises focused interviews with the (Wurundjeri (Yarra Valley), Wathaurong Geelong-Bellarine Peninsular) & Boon Wurrung (Mornington Peninsula)) to elicit a contemporary and local response to issues raised by NCCARF but importantly to articulate a possible Indigenous position about the formation, change and direction that Port Phillip Bay and its environs should take from their perspectives. Research draws upon how these communities have adapted to climate change physically, mentally and spiritually over their long habitation of a shared geological asset and their perceptions of climate change in respect to forecasting and adapting to climate change for this century. The project looks to uncover a longitudinal perspective of change and adaptation focused upon Indigenous views of ‘country’ and traditional custodial obligations to ‘country’ including accumulated cultural and environmental histories.

Mikrosomale Biotransformation von Benzo[ghi]perylen, einem mutagenen polyaromatischen Kohlenwasserstoff ohne das Strukturelement der Bay-Region des kanzerogenen Benzo[a]pyrens

Kanzerogene polyaromatische Kohlenwasserstoffe (PAKs), wie Benzo[a]pyren, besitzen eine Bay-Region mit ortho-kondensiertem Benzoring. Dadurch ist die enzymatische Bildung von Bay-Region-Dihydrodiolepoxiden (Oxiranylring in der sterisch abgeschirmten Molekülbucht) möglich, die als ultimal kanzerogene Metaboliten der PAKs gelten. Diese lösen durch DNA-Modifikation Primärläsionen aus, die, sofern sie nicht enzymatisch repariert werden, bei der DNA-Replikation Fehler verursachen (Mu-tationen). Der Mehrstufenprozeß der Kanzerogenese (Promotion und Progression) führt schließlich zur neoplastischen Entartung der Zelle. Benzo[ghi]perylen (BghiP) repräsentiert eine Gruppe von PAKs, die keine „klassische“ Bay-Region besitzen und daher keine vicinalen Dihydrodiolepoxiden bilden können. Trotzdem ist BghiP mutagen, z. B. in den Stämmen TA98 und TA100 von Salmonella typhimurium (1,3- bzw. 4,3 his+-Revertanten/nmol) nach metabolischer Aktivierung mit der postmitochondrialen Fraktion von Ratten nach Behandlung mit 3-Methylcholanthren. Hemmung der mikrosomalen Epoxidhydrolase (mEH) mit 1,1,1-Trichlor-2-propenoxid (TCPO) steigert die bakterielle Mutagenität von BghiP im Stamm TA98 um das 4-fache, was Arenoxide als ultimale Mutagene wahrscheinlich macht. Dieses Ergebnis wird au-ßerdem durch Untersuchung der DNA-Bindung mit dem Verfahren des 32P-Postlabelings bestätigt (Dr. Fickler, Institut für Toxikologie, Universität Mainz). Danach bildete mikrosomal aktiviertes BghiP drei Addukte (ein Hauptaddukt, zwei Nebenaddukte), die durch Hemmung der mEH mit TCPO verstärkt wurden (das Hauptaddukt um 29%). Um den für die bakterielle Mutagenität von BghiP verantwortlichen Metaboliten zu identifizieren, wurde die mikrosomale Biotransformaton von BghiP aufgeklärt. Umsetzung von BghiP mit Lebermikrosomen von Ratten nach Behandlung mit Aroclor 1254 lieferte 17 mit Ethylacetat extrahierbare Metaboliten. Zwölf dieser Metaboliten konnten durch eine Kombination von chromatographischen, spektroskopi-schen und biochemischen Methoden identifiziert werden. Daraus ergeben sich zwei Biotransformati-onswege: Weg I beginnt mit einem Angriff von Cytochrom P450-abhängigen Monooxygenasen an Position 7 und der Bildung des 7-Phenols. Dieses wird dann in das 7,8- bzw. 7,10-Diphenol überführt, die schließlich zu den mehrkernigen Chinonen an der 7,8- bzw. 7,10-Position oxidiert werden. Im Bio-transformationsweg II werden die K-Regionen von BghiP durch Cytochrom P450 funktionalisiert. Zu-nächst entstehen das auf indirektem Weg identifizierte 3,4-Oxid und das 3,4,11,12-Bisoxid, die in mikrosomalen Umsetzungen von BghiP nur nach Hemmung der mEH gebildet werden. Enzymatische Hydrolyse des 3,4-Oxides ergibt das trans-3,4-Dihydrodiol, das zum 3,4-Chinon oxidiert wird. Ebenso entsteht aus dem 3,4,11,12-Bisoxid das trans-3,4-trans-11,12-Bisdihydrodiol, aus dem durch Oxidati-on das trans-3,4-Dihydrodiol-11,12-Chinon hervorgeht. Untersuchung der stereoselektiven enzymati-schen Bildung der K-Region-trans-Di¬hydrodiole ergaben eine präferentielle Entstehung der 3R,4R- bzw. 3R,4R,11R,12R-Enantiomere. Untersuchungen der bakteriellen Mutagenität der Hauptmetaboliten 3,4-Dihydrodiol und dem 7-Phenol machte deutlich, dass beide Biotransformationswege I und II von BghiP zur bakteriellen Mutagenität beitragen. Das 7-Phenol aus Weg I ist ein proximales Mutagen, was auch von Phenolen anderer PAKs bekannt ist. Das 3,4-Dihydrodiol aus Weg II wird so schwach zu Mutagenen aktiviert, dass dem vermutlich gebildete 3,4-Dihydrodiol-11,12-oxid keine große Bedeutung als ultimales Mutagen von BghiP zukommt. Die Bestimmung der direkten mutagenen Aktivität (ohne metabolische Aktivierung) der mutmaßlich ultimal mutagenen Arenoxide von BghiP ergab, dass die des 3,4,11,12-Bisarenoxides sehr gering war (1,3 his+-Revertanten/nmol im Stamm TA98). Das 3,4-Oxid hingegen bewirkte einen deutlichen gentoxischen Effekt in den Stämmen TA98 und TA100 (5,5 bzw. 10 his+-Revertanten/nmol). Dies wurde durch die Bestimmung der DNA-Bindung mit dem 32P-Postlabeling, in dem das 3,4-Oxid für das Hauptaddukt von BghiP verantwortlich gemacht werden konnte, bestätigt. Daher kommt dem 3,4-Oxid als ultimales Mutagen die größte Bedeutung für die Gentoxizität von BghiP zu. Die Ergebnisse dieser Arbeit lassen bei PAKs ohne Bay-Region auf Arenoxide schließen, die eine notwendige Voraussetzung für DNA-Bindung und Mutagenität sind.