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  • 1
    Online Resource
    Online Resource
    Cham : Springer International Publishing AG
    Keywords: Electronic books
    Description / Table of Contents: Liquidity, Markets and Trading in Action -- Preface -- Microeconomics, Chap. 1 -- Finance, Chap. 2 -- Macroeconomics, Chap. 3 -- Information Systems, Chap. 4 -- Simulated Trading, Chap. 5 -- Aim of This Book -- Acknowledgment -- Contents -- 1: Economics and the Equity Market: A Microeconomics Course Application -- 1.1 Microeconomics in a Nutshell -- 1.2 Microeconomic Analysis Goes to an Equity Market -- 1.3 Risk, Return Indifference Curves -- 1.4 The Constraint -- 1.5 Demand Curve to Hold Shares of the Market Portfolio -- 1.6 What About the Supply Curve? -- 1.7 Buy and Sell Curves -- 1.8 The Non-frictionless Market -- 1.9 Wrap Up: Microeconomics in a Non-frictionless Financial Market -- 2: Liquidity, Trading, and Price Determination in Equity Markets: A Finance Course Application -- 2.1 Order Types -- 2.2 Trading Costs -- 2.3 What Drives Trading? -- 2.4 Price Discovery: A Major Function of a Marketplace -- 2.5 Trading: The Implementation of an Investment Decision -- 2.6 Intraday Price Volatility -- 2.7 Liquidity -- 2.8 Equity Market Structures -- 2.8.1 Hybrid Markets -- 2.8.2 Handling Large Orders -- 2.9 Financial Markets and the Process of Turning Orders into Trades -- 2.9.1 Trades in Continuous Order-Driven Markets -- 2.9.2 Trades in Call Auction Markets -- 2.9.3 Trades in Continuous Dealer Markets -- 2.10 Regulation, Technology, and the Quality of Market Structure -- 2.11 Wrapping It Up: Market Efficiency in a Non-frictionless World -- 3: Liquidity and the Impact of Information Shocks: A Macroeconomics Course Application -- 3.1 Economic Conditions, Business Cycles, and the Role of Interest Rates -- 3.2 The Federal Reserve and the Link Between the Macroeconomy and Financial Markets -- 3.3 The Impact of Information Shocks on Divergent Expectations and Price Discovery -- 3.4 The Various Types of Financial Markets.
    Type of Medium: Online Resource
    Pages: 1 online resource (111 pages)
    ISBN: 9783030748173
    Series Statement: Classroom Companion: Business Ser.
    Language: English
    Note: Description based on publisher supplied metadata and other sources
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  • 2
    Online Resource
    Online Resource
    Cham : Springer International Publishing AG
    Type of Medium: Online Resource
    Pages: 1 online resource (639 pages)
    Edition: 2nd ed.
    ISBN: 9783031231940
    DDC: 332.09494
    Language: English
    Note: Description based on publisher supplied metadata and other sources
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  • 3
    Publication Date: 2024-02-07
    Description: Many studies show the sensitivity of our environment to manmade changes, especially the anthropogenic impact on atmospheric and hydrological processes. The effect on Solid Earth processes such as subsidence is less straightforward. Subsidence is usually slow and relates to the interplay of complex hydro-mechanical processes, thus making relations to atmospheric changes difficult to observe. In the Dead Sea (DS) region, however, climatic forcing is strong and over-use of fresh water is massive. An observation period of 3 years was thus sufficient to link the high evaporation (97 cm/year) and the subsequent drop of the Dead Sea lake level (− 110 cm/year), with high subsidence rates of the Earth’s surface (− 15 cm/year). Applying innovative Global Navigation Satellite System (GNSS) techniques, we are able to resolve this subsidence of the “Solid Earth” even on a monthly basis and show that it behaves synchronous to atmospheric and hydrological changes with a time lag of two months. We show that the amplitude and fluctuation period of ground deformation is related to poro-elastic hydro-mechanical soil response to lake level changes. This provides, to our knowledge, a first direct link between shore subsidence, lake-level drop and evaporation.
    Type: Article , PeerReviewed
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  • 4
    Publication Date: 2024-02-07
    Description: The Southern Ocean paleoceanography provides key insights into how iron fertilization and oceanic productivity developed through Pleistocene ice-ages and their role in influencing the carbon cycle. We report a high-resolution record of dust deposition and ocean productivity for the Antarctic Zone, close to the main dust source, Patagonia. Our deep-ocean records cover the last 1.5 Ma, thus doubling that from Antarctic ice-cores. We find a 5 to 15-fold increase in dust deposition during glacials and a 2 to 5-fold increase in biogenic silica deposition, reflecting higher ocean productivity during interglacials. This antiphasing persisted throughout the last 25 glacial cycles. Dust deposition became more pronounced across the Mid-Pleistocene Transition (MPT) in the Southern Hemisphere, with an abrupt shift suggesting more severe glaciations since ~0.9 Ma. Productivity was intermediate pre-MPT, lowest during the MPT and highest since 0.4 Ma. Generally, glacials experienced extended sea-ice cover, reduced bottom-water export and Weddell Gyre dynamics, which helped lower atmospheric CO2 levels.
    Type: Article , PeerReviewed , info:eu-repo/semantics/article
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  • 5
    Publication Date: 2024-02-07
    Description: Antarctica is one of the most vulnerable regions to climate change on Earth and studying the past and present responses of this polar marine ecosystem to environmental change is a matter of urgency. Sedimentary ancient DNA (sedaDNA) analysis can provide such insights into past ecosystem-wide changes. Here we present authenticated (through extensive contamination control and sedaDNA damage analysis) metagenomic marine eukaryote sedaDNA from the Scotia Sea region acquired during IODP Expedition 382. We also provide a marine eukaryote sedaDNA record of ~1 Mio. years and diatom and chlorophyte sedaDNA dating back to ~540 ka (using taxonomic marker genes SSU, LSU, psbO). We find evidence of warm phases being associated with high relative diatom abundance, and a marked transition from diatoms comprising 〈10% of all eukaryotes prior to ~14.5 ka, to ~50% after this time, i.e., following Meltwater Pulse 1A, alongside a composition change from sea-ice to open-ocean species. Our study demonstrates that sedaDNA tools can be expanded to hundreds of thousands of years, opening the pathway to the study of ecosystem-wide marine shifts and paleo-productivity phases throughout multiple glacial-interglacial cycles.
    Type: Article , PeerReviewed
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