Analysis of minerals from Arctic Ocean sediments

The Arctic Ocean System is a key player regarding the climatic changes of Earth. Its highly sensitive ice Cover, the exchange of surface and deep water masses with the global ocean and the coupling with the atmosphere interact directly with global climatic changes. The output of cold, polar water and sea ice influences the production of deep water in the North Atlantic and controls the global ocean circulation ("the conveyor belt"). The Arctic Ocean is surrounded by the large Northern Hemisphere ice sheets which not only affect the sedimentation in the Arctic Ocean but also are supposed to induce the Course of glacials and interglacials. Terrigenous sediment delivered from the ice sheets by icebergs and meltwater as well as through sea ice are major components of Arctic Ocean sediments. Hence, the terrigenous content of Arctic Ocean sediments is an outstanding archive to investigate changes in the paleoenvironment. Glazigenic sediments of the Canadian Arctic Archipelago and surface samples of the Arctic Ocean and the Siberian shelf regions were investigated by means of x-ray diffraction of the bulk fraction. The source regions of distinct mineral compositions were to be deciphered. Regarding the complex circumpolar geology stable christalline shield rocks, active and ancient fold belts including magmatic and metamorphic rocks, sedimentary rocks and wide periglacial lowlands with permafrost provide a complete range of possible mineral combinations. Non- glaciated shelf regions mix the local input from a possible point source of a particular mineral combination with the whole shelf material and function as a sampler of the entire region draining to the shelf. To take this into account, a literature research was performed. Descriptions of outcropping lithologies and Arctic Ocean sediments were scanned for their mineral association. The analyses of glazigenic and shelf sediments yielded a close relationship between their mineral composition and the adjacent source region. The most striking difference between the circumpolar source regions is the extensive outcrop of carbonate rocks in the vicinity of the Canadian Arctic Archipelago and in N Greenland while siliciclastic sediments dominate the Siberian shelves. In the Siberian shelf region the eastern Kara Sea and the western Laptev Sea form a destinct region defined by high smectite, (clino-) pyroxene and plagioclase input. The source of this signal are the extensive outcrops of the Siberian trap basalt in the Putorana Plateau which is drained by the tributaries of the Yenissei and Khatanga. The eastern Laptev Sea and the East Siberian Sea can also be treated as one source region containing a feldspar, quartz, illite, mica, and chlorite asscciation combined with the trace minerals hornblende and epidote. Franz Josef Land provides a mineral composition rich in quartz and kaolinite. The diverse rock suite of the Svalbard archipelago distributes specific mineral compositions of highly metamorphic christalline rocks, dolomite-rich carbonate rocks and sedimentary rocks with a higher diagenetic potential manifested in stable newly built diagenetic minerals and high organic maturity. To reconstruct the last 30,000 years as an example of the transition between glacial and interglacial conditions a profile of sediment cores, recovered during the RV Polarstern" expedition ARK-VIIIl3 (ARCTIC '91), and additional sediment cores around Svalbard were investigated. Besides the mineralogy of different grain size fractions several additional sedimentological and organo-geochemical Parameterswere used. A detailed stratigraphic framework was achieved. By exploiting this data set changes in the mineral composition of the Eurasian Basin sediments can be related to climatic changes. Certain mineral compositions can even be associated with particular transport processes, e.g. the smectitel pyroxene association with sea ice transport from the eastern Kara Sea and the western Laptev Sea. Hence, it is possible to decipher the complex interplay between the influx of warm Atlantic waters into the Southwest of the Eurasian Basin, the waxing and waning of the Svalbard1Barents- Sea- and Kara-Sea-Ice-Sheets, the flooding of the Siberian shelf regions and the surface and deep water circulation. Until now the Arctic Ocean was assumed to be a rather stable System during the last 30,000 years which only switched from a completely ice covered situation during the glacial to seasonally Open waters during the interglacial. But this work using mineral assemblages of sediment cores in the vicinity of Svalbard revealed fast changes in the inflow of warm Atlantic water with the Westspitsbergen Current (< 1000 years), short periods of advances and retreats of the marine based Eurasian ice sheets (1000-3000 years), and short melting phases (400 years?). Deglaciation of the marine-based Eurasian and the land-based north American and Greenland ice sheets are not simultaneous. This thesis postulates that the Kara Sea Ice Sheet released an early meltwater signal prior to 15,000 14C years leading the Barents Sea Ice Sheet while the western land-based ice sheets are following later than 13,500 14C years. The northern Eurasian Basin records the shift between iceberg and sea-ice material derived from the Canadian Arctic Archipelago and N-Greenland and material transported by sea-ice and surface currents from the Siberian shelf region. The phasing of the deglaciation becomes very obvious using the dolomite and quartd phyllosilicate record. It is also supposed that the flooding of the Laptev Sea during the Holocene is manifested in a stepwise increase of sediment input at the Lomonosov Ridge between the Eurasian and Amerasian Basin. Depending on the strength of meltwater pulses from the adjacent ice sheets the Transpolar Drift can probably be relocated. These movements are traceable by the distribution of indicator minerals. Based on the outcome of this work the feasibility of bulk mineral determination can be qualified as excellent tool for paleoenvironmental reconstructions in the Arctic Ocean. The easy preparation and objective determination of bulk mineralogy provided by the QUAX software bears the potential to use this analyses as basic measuring method preceding more time consuming and highly specialised mineralogical investigations (e.g. clay mineralogy, heavy mineral determination).

The role of the G20 in WTO governance

Report by Professor Sungjoon Cho, Associate Professor of Law, Chicago-Kent College of Law (Chair), and Charlotte Sieber-Gasser, Doctoral Research Fellow, World Trade Institute, University of Bern, Session 27, WTO Public Forum 2010: The Forces Shapping World Trade, pp.29-33. In the course of the financial crisis, the global geography of power has shifted from G8 to G20. The latter, although representing roughly two thirds of global trade, consists of relatively a small number of global players and is consequently excluding many others from decision-making at the international stage. Nevertheless, the G20 has been successful in its reaction to the financial crisis and became therewith an important new player within the international community. When highlighting how the G20 might interfere with the WTO, the panel voiced concerns over the political legitimacy of the G20, given the limited number of members and the global impact of its decisions. It agreed on the impression that although the G20 intends to extend its debates from the financial sector to world economy in general, it has so far little achieved in this direction, particularly when it comes to moving the Doha agenda forward. It remains, thus, open how the G20 will evolve in the coming few years, and what mandates it will shed or adopt. So far, the G20 has complemented the WTO and international financial institutions in handling the financial crisis. Yet, even if there is little evidence pointing towards a less cooperative role in the future, the desirability of a G20 commitment in WTO trade negotiations has yet to be debated. The panel concluded by providing ideas on how the potential of the G20 might be used to serve global interests even better in the future. In their concluding remarks, the panellists agreed that it remains to be seen whether or not the G20 will further broaden its agenda. Given the ebbing away of the financial crisis there is even the question whether the G20 will remain an important international forum for financial collaboration, or whether it has already served its cause and will eventually disappear from the international stage. The Chair concluded the well attended and lively panel with voicing the hope that the two international bodies – the G20 and the WTO – will work in a positive way together in the future and face the challenges and opportunities in their collaboration to the benefit of everyone.

Tom Harmon, 1939, UM Men's basketball

[probably as intramural rather than varsity player)

Kathryn Gleason and U-M softball coaches, 1995 NCAA Regional

[Player introductions, DePaul game]

Kathryn Gleason and U-M softball coaches, 1995 NCAA Regional

[Player introductions, DePaul game]

Tom Harmon, UM Football, carrying ball vs Ohio State 1940

[blocking for Harmon L-R: Albert Wistert (11), Ed Frutig (87), Ralph Fritz (63), Bob Westfall (86), Robert Ingalls (66) OSU player is Thomas Kinkade (16)

UM Football vs Ohio State, 1989

[James Williams (17), Chris Bohn (49) and Brian Townsend (45) tackle OSU player]

Dennis Fitzgerald, UM football, 1961, in leather helmet

[Fitzgerald was last Michigan player to wear a leather helmet. Pictured holding the model worn by other players, says leather helmet fits better and gives him more freedom of movement. (from note in neg. envelope.)]

Catalog of metrostyle and themodist music for the pianola and pianola piano : containing a complete list of all numbers issued to July, 1906.

Mode of access: Internet.

The theatre.

Description based on surrogate; title from cover.

Chess and checkers : the way to mastership /

"Complete instructions for the beginner, valuable suggestions for the advanced player."

The school of Shakspere.

Completed after the editor's death by J.W.M. Gibbs and Dr. Furnivall. cf. Notice, signed F.J. Furnivall.