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  • 1
    Call number: PIK B 020-94-0223
    In: Wiley series in probability and statistics
    Type of Medium: Monograph available for loan
    Pages: 1019 p.
    Edition: 2. Aufl.
    ISBN: 047189530x
    Series Statement: Wiley series in probability and mathematical statistics
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 2
    Call number: PIK B 020-18-91415
    Description / Table of Contents: enth.
    Type of Medium: Monograph available for loan
    Pages: XVI, 307 Seiten , Diagramme, Tabellen
    Edition: Reprinted
    ISBN: 0471953113
    Series Statement: Series in financial economics and quantitative analysis
    Language: English
    Note: Contents: Introduction ; The Classical Maximum Entropy Formalism: A Review ; PURE INVERSE PROBLEMS ; Basic Maximum Entropy Principle: Formulation and Extensions ; Formulation and Solution of Pure Inverse Problems ; Generalized Pure Inverse Problems ; LINEAR INVERSE PROBLEMS WITH NOISE ; Generalized Maximum Entropy (GME) and Cross-Entropy (GCE) Formulations ; Finite Sample Extensions of GME-GCE ; GENERAL LINEAR MODEL APPLICATIONS OF GME-GCE ; GME-GCE Solutions to Ill-conditioned Problems ; General Linear Statistical Model with a Non-scalar Identity Covariance Matrix Statistical Model Selection ; A SYSTEM OF ECONOMIC STATISTICAL RELATIONS ; Sets of Linear Statistical Models ; Simultaneous Equations Statistical Model ; LINEAR AND NON-LINEAR DYNAMIC SYSTEMS ; Estimation and Inference of Dynamic Linear Inverse Problems ; Linear and Non-linear Dynamic Systems with Control ; DISCRETE CHOICE-CENSORED PROBLEMS ; Recovering Information from Multinomial Response Data ; Recovering Information from Censored Response Data ; COMPUTATIONAL NOTES ; Computing GME-GCE Solutions ; Epilogue
    Location: A 18 - must be ordered
    Branch Library: PIK Library
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  • 3
    Publication Date: 2020-02-17
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 4
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    PANGAEA
    In:  Supplement to: Pauly, George G; van Vleet, Edward S (1985): Archaebacterial ether lipids: Natural tracers of biogeochemical processes. Organic Geochemistry, 10(4-6), 859-867, https://doi.org/10.1016/S0146-6380(86)80023-7
    Publication Date: 2023-06-27
    Description: Methanogen ether lipids have been quantified in sediments from a Florida swamp and the Atlantic ocean. Swamp cores containing acyclic and monocyclic isopranyl ethers are clearly differentiated from deep sea sediments which also contain bicyclic compounds. A concentration maximum near the bottom of the sulfate reducing zone in deep sea sediments may reflect a biogeochemical system in which methanogenesis and sulfate reduction are coupled by the process of methane oxidation. Lipid diagenesis is evident in the deep sea sediments. Species zonation, possibly caused by oxygen sensitivity, is detected in the relative lipid abundances in swamp sediments.
    Keywords: 75-532B; 93-603B; DRILL; Drilling/drill rig; Florida; Glomar Challenger; HPC; Hydraulic piston corer; Lake_Maggiore_3; Lake_Maggiore_4; Leg75; Leg93; LM3; LM4; South Atlantic
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 5
    Publication Date: 2023-06-27
    Keywords: Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Ether lipid C20 per unit sediment mass; Ether lipid C40-0 per unit sediment mass; Ether lipid C40-1* per unit sediment mass; Ether lipid C40-1 per unit sediment mass; Ether lipids per unit sediment mass; Event label; Florida; HPC; Hydraulic piston corer; Lake_Maggiore_3; Lake_Maggiore_4; LM3; LM4
    Type: Dataset
    Format: text/tab-separated-values, 125 data points
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  • 6
    Publication Date: 2023-06-27
    Keywords: 75-532B; 93-603B; AGE; Age, maximum/old; Age, minimum/young; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Ether lipid C40-0 per unit sediment mass; Ether lipid C40-1 per unit sediment mass; Ether lipid C40-2* per unit sediment mass; Ether lipid C40-2 per unit sediment mass; Ether lipids per unit sediment mass; Event label; Glomar Challenger; Leg75; Leg93; Sample code/label; South Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 44 data points
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  • 7
    Publication Date: 2023-06-27
    Keywords: 75-532B; 93-603B; AGE; Age, maximum/old; Age, minimum/young; Alcohols per unit sediment mass; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Ether lipids per unit sediment mass; Event label; Glomar Challenger; Leg75; Leg93; Lipids, polar per unit sediment mass; Sample code/label; South Atlantic
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 8
    Publication Date: 2023-10-26
    Description: Ocean acidification (OA)—a process describing the ocean's increase in dissolved carbon dioxide ( pCO2) and a reduction in pH and aragonite saturation state (Ωar) due to higher concentrations of atmospheric CO2—is considered a threat to bivalve mollusks and other marine calcifiers. While many studies have focused on the effects of OA on shell formation and growth, we present findings on the separate effects of pCO2, Ωar, and pH on larval feeding physiology (initiation of feeding, gut fullness, and ingestion rates) of the California mussel Mytilus californianus. We found that elevated pCO2 delays initiation of feeding, while gut fullness and ingestion rates were best predicted by Ωar; however, pH was not found to have a significant effect on these feeding processes under the range of OA conditions tested. We also modeled how OA impacts on initial shell development and how feeding physiology might subsequently affect larval energy budget components (e.g. scope for growth) and developmental rate to 260 µm shell length, a size at which larvae typically become pediveligers. Our model predicted that Ωar impacts on larval shell size and ingestion rates over the initial 48 h period of development would result in a developmental delay to the pediveliger stage of 〉4 d, compared with larvae initially developing in supersaturated conditions (Ωar 〉 1). Collectively, these results suggest that predicted increases in pCO2 and reduced Ωar values may negatively impact feeding activity and energy balances of bivalve larvae, reducing their overall fitness and recruitment success.
    Keywords: Alkalinity, total; Animalia; Aragonite saturation state; Behaviour; Bicarbonate ion; Bottles or small containers/Aquaria (〈20 L); Calcite saturation state; Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Coast and continental shelf; EXP; Experiment; Feeding rate; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Gut fullness, size standardized; Gut fullness, total beads per larva; Ingestion rate per larva; Ingestion rate per larva, size standardized; Laboratory experiment; Larvae; Mollusca; Mytilus californianus; North Pacific; Number; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Pelagos; pH; Replicate; Salinity; Seal_Rock; Single species; Size; Species, unique identification; Temperate; Temperature, water; Treatment; Type of study; Zooplankton
    Type: Dataset
    Format: text/tab-separated-values, 1632 data points
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  • 9
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    PANGAEA
    In:  Supplement to: Pérez, Claudia; Lagos, Nelson A; Saldias, Gonzalo S; Waldbusser, George G; Vargas, C A (2016): Riverine discharges impact physiological traits and carbon sources for shell carbonate in the marine intertidal mussel Perumytilus purpuratus. Limnology and Oceanography, 61(3), 969-983, https://doi.org/10.1002/lno.10265
    Publication Date: 2024-03-20
    Description: Anthropogenic modification watersheds and climate change have altered export from fluvial systems causing changes to the carbonate chemistry of river-influenced near shore environments. To determine the possible effects of riverine discharges on the mussel Perumytilus purpuratus, we performed in situ transplant experiments between river-influenced and open coastal habitats with contrasting seawater carbonate chemistries (i.e., pCO2, pH, Omega ar) across four regions covering a wide latitudinal range (32°55'S-40°10'S). The river-influenced habitats selected for transplant experiments were different than open coastal habitats; with higher pCO2 (354-1313 µatm), lower pH (7.6?7.9) and Omega ar values (0.4?1.4) than in open coastal area. Growth, calcification, metabolism were measured in a reciprocal transplant experiment to determine physiological responses associated with river-influenced sites and non-influenced control sites. Growth and calcification rates were higher in river-influenced habitats; however the organisms in this area also had lower metabolic rates, possibly due to enhanced food supply from river systems. Further analysis of carbon isotopic composition (delta 13C) indicated that the relative contribution of seawater dissolved inorganic carbon (DIC) to the carbonate shells of P. purpuratus was much higher than respiratory carbon. Nevertheless, P. purpuratus incorporated between 7% and 26% of metabolic carbon in the shell depending on season. There was a strong, significant relationship between delta 13C POC and delta 13C Tissue, which likely influenced the isotopic composition of the shell carbon.
    Keywords: Alkalinity, total; Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Brackish waters; Calcification/Dissolution; Calcification rate, standard deviation; Calcite saturation state; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Estuary; Field experiment; Figure; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Growth/Morphology; Growth rate; Growth rate, standard deviation; Location; Metabolic rate of oxygen; Metabolic rate of oxygen, standard deviation; Mollusca; Month; Net calcification rate of calcium carbonate, per individual; OA-ICC; Ocean Acidification International Coordination Centre; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); Percentage; Perumytilus purpuratus; pH; Potentiometric; Potentiometric titration; Registration number of species; Respiration; Salinity; Single species; Site; South Pacific; Species; Temperate; Temperature, water; Treatment; Type; Uniform resource locator/link to reference; δ13C, dissolved inorganic carbon; δ13C, particulate inorganic carbon; δ13C, particulate organic carbon
    Type: Dataset
    Format: text/tab-separated-values, 2066 data points
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  • 10
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    PANGAEA
    In:  Supplement to: Waldbusser, George G; Voigt, Erin P; Bergschneider, Heather; Green, Mark A; Newell, Roger I E (2011): Biocalcification in the Eastern Oyster (Crassostrea virginica) in Relation to Long-term Trends in Chesapeake Bay pH. Estuaries and Coasts, 34(2), 221-231, https://doi.org/10.1007/s12237-010-9307-0
    Publication Date: 2024-03-15
    Description: Anthropogenic carbon dioxide (CO2) emissions reduce pH of marine waters due to the absorption of atmospheric CO2 and formation of carbonic acid. Estuarine waters are more susceptible to acidification because they are subject to multiple acid sources and are less buffered than marine waters. Consequently, estuarine shell forming species may experience acidification sooner than marine species although the tolerance of estuarine calcifiers to pH changes is poorly understood. We analyzed 23 years of Chesapeake Bay water quality monitoring data and found that daytime average pH significantly decreased across polyhaline waters although pH has not significantly changed across mesohaline waters. In some tributaries that once supported large oyster populations, pH is increasing. Current average conditions within some tributaries however correspond to values that we found in laboratory studies to reduce oyster biocalcification rates or resulted in net shell dissolution. Calcification rates of juvenile eastern oysters, Crassostrea virginica, were measured in laboratory studies in a three-way factorial design with 3 pH levels, two salinities, and two temperatures. Biocalcification declined significantly with a reduction of ~0.5 pH units and higher temperature and salinity mitigated the decrease in biocalcification.
    Keywords: Alkalinity, total; Alkalinity anomaly technique (Smith and Key, 1975); Animalia; Aragonite saturation state; Benthic animals; Benthos; Bicarbonate ion; Bottles or small containers/Aquaria (〈20 L); Brackish waters; Calcification/Dissolution; Calcification rate, standard deviation; Calcification rate of calcium carbonate; Calcite saturation state; Calculated; Calculated using CO2SYS; Calculated using seacarb after Nisumaa et al. (2010); Carbon, inorganic, dissolved; Carbonate ion; Carbonate system computation flag; Carbon dioxide; Crassostrea virginica; EPOCA; EUR-OCEANS; European network of excellence for Ocean Ecosystems Analysis; European Project on Ocean Acidification; Experimental treatment; Fugacity of carbon dioxide (water) at sea surface temperature (wet air); Laboratory experiment; Mollusca; North Atlantic; OA-ICC; Ocean Acidification International Coordination Centre; Orion Ross conductivity probe; Partial pressure of carbon dioxide (water) at sea surface temperature (wet air); pH; Salinity; Single species; Species; Temperate; Temperature; Temperature, water; Two-point titration (Edmond 1970)
    Type: Dataset
    Format: text/tab-separated-values, 376 data points
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