@article{Fery2007,
  author    = {F{\´e}ry, Caroline},
  title     = {Information structural notions and the fallacy of invariant correlates},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-19692},
  year      = {2007},
  abstract  = {In a first step, definitions of the irreducible information structural categories are given, and in a second step, it is shown that there are no invariant phonological or otherwise grammatical correlates of these categories. In other words, the phonology, syntax or morphology are unable to define information structure. It is a common mistake that information structural categories are expressed by invariant grammatical correlates, be they syntactic, morphological or phonological. It is rather the case that grammatical cues help speaker and hearer to sort out which element carries which information structural role, and only in this sense are the grammatical correlates of information structure important. Languages display variation as to the role of grammar in enhancing categories of information structure, and this variation reflects the variation found in the 'normal' syntax and phonology of languages.},
  language  = {en}
}
@article{EndrissHinterwimmer2007,
  author    = {Endriss, Cornelia and Hinterwimmer, Stefan},
  title     = {Direct and indirect aboutness topics},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-19640},
  year      = {2007},
  abstract  = {We propose a definition of aboutness topicality that not only encompasses individual denoting DPs, but also indefinites. We concentrate on the interpretative effects of marking indefinites as topics: they either receive widest scope in their clause, or they are interpreted in the restrictor of an overt or covert Q-adverb. We show that in the first case they are direct aboutness topics insofar as they are the subject of a predication expressed by the comment, while in the second case they are indirect aboutness topics: they define the subject of a higher-order predication - namely the set of situations that the respective Q-adverb quantifies over.},
  language  = {en}
}
@article{Kasimir2006,
  author    = {Kasimir, Elke},
  title     = {On 'nicht...sondern...' (contrastive 'not...but...')},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-19537},
  year      = {2006},
  abstract  = {This article presents an analysis of German nicht...sondern... (contrastive not...but...) which departs from the commonly held view that this construction should be explained by appeal to its alleged corrective function. It will be demonstrated that in nicht A sondern B (not A but B), A and B just behave like stand-alone unmarked answers to a common question Q, and that this property of sondern is presuppositional in character. It is shown that from this general observation many interesting properties of nicht...sondern... follow, among them distributional differences between German 'sondern' and German 'aber' (contrastive but, concessive but), intonational requirements and exhaustivity effects. sondern's presupposition is furthermore argued to be the result of the conventionalization of conversational implicatures.},
  language  = {en}
}
@article{vandeVijverSennemaZimmer–Stahl2006,
  author    = {van de Vijver, Ruben and Sennema, Anke and Zimmer-Stahl, Anne},
  title     = {An analysis of pitch and duration in material used to test L2 processing of words},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-19583},
  year      = {2006},
  abstract  = {The material reported on in this paper is part of a set of experiments in which the role of Information Structure on L2 processing of words is tested. Pitch and duration of 4 sets of experimental material in German and English are measured and analyzed in this paper. The well-known finding that accent boosts duration and pitch is confirmed. Syntactic and lexical means of marking focus, however, do not give the duration and the pitch of a word an extra boost.},
  language  = {en}
}
@article{SchmitzHoehleMuelleretal.2006,
  author    = {Schmitz, Michaela and H{\"o}hle, Barbara and M{\"u}ller, Anja and Weissenborn, J{\"u}rgen},
  title     = {The recognition of the prosodic focus position in German-learning infants from 4 to 14 months},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-19566},
  year      = {2006},
  abstract  = {The aim of the present study was to elucidate in a study with 4-, 6-, 8-, and 14-month-old German-learning children, when and how they may acquire the regularities which underlie Focus-to-Stress Alignment (FSA) in the target language, that is, how prosody is associated with specific communicative functions. Our findings suggest, that 14-month-olds have already found out that German allows for variable focus positions, after having gone through a development which goes from a predominantly prosodically driven processing of the input to a processing where prosody interacts more and more with the growing lexical and syntactic knowledge of the child.},
  language  = {en}
}
@article{EndrissHinterwimmer2006,
  author    = {Endriss, Cornelia and Hinterwimmer, Stefan},
  title     = {Quantificational Variability Effects with plural definites},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-19512},
  year      = {2006},
  abstract  = {In this paper we compare the behaviour of adverbs of frequency (de Swart 1993) like usually with the behaviour of adverbs of quantity like for the most part in sentences that contain plural definites. We show that sentences containing the former type of Q-adverb evidence that Quantificational Variability Effects (Berman 1991) come about as an indirect effect of quantification over situations: in order for quantificational variability readings to arise, these sentences have to obey two newly observed constraints that clearly set them apart from sentences containing corresponding quantificational DPs, and that can plausibly be explained under the assumption that quantification over (the atomic parts of) complex situations is involved. Concerning sentences with the latter type of Q-adverb, on the other hand, such evidence is lacking: with respect to the constraints just mentioned, they behave like sentences that contain corresponding quantificational DPs. We take this as evidence that Q-adverbs like for the most part do not quantify over the atomic parts of sum eventualities in the cases under discussion (as claimed by Nakanishi and Romero (2004)), but rather over the atomic parts of the respective sum individuals.},
  language  = {en}
}
@article{HellmuthSkopeteas2007,
  author    = {Hellmuth, Sam and Skopeteas, Stavros},
  title     = {Information structure in linguistic theory and in speech production : validation of a Cross-Linguistic data set},
  publisher = {Universit{\"a}tsverlag Potsdam},
  address   = {Potsdam},
  isbn      = {978-3-939469-72-8},
  issn      = {1866-4725},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-19450},
  pages     = {141 -- 186},
  year      = {2007},
  abstract  = {The aim of this paper is to validate a dataset collected by means of production experiments which are part of the Questionnaire on Information Structure. The experiments generate a range of information structure contexts that have been observed in the literature to induce specific constructions. This paper compares the speech production results from a subset of these experiments with specific claims about the reflexes of information structure in four different languages. The results allow us to evaluate and in most cases validate the efficacy of our elicitation paradigms, to identify potentially fruitful avenues of future research, and to highlight issues involved in interpreting speech production data of this kind.},
  language  = {en}
}
@article{KueglerSkopeteasVerhoeven2007,
  author    = {K{\"u}gler, Frank and Skopeteas, Stavros and Verhoeven, Elisabeth},
  title     = {Encoding information structure in Yucatec Maya},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-19469},
  year      = {2007},
  abstract  = {The aim of this paper is to outline the means for encoding information structure in Yucatec Maya. Yucatec Maya is a tone language, displaying a three-fold opposition in the tonal realization of syllables. From the morpho-syntactic point of view, the grammar of Yucatec Maya contains morphological (topic affixes, morphological marking of out-of-focus predicates) and syntactic (designated positions) means to uniquely specify syntactic constructions for their information structure. After a descriptive overview of these phenomena, we present experimental evidence which reveals the impact of the nonavailability of prosodic alternatives on the choice of syntactic constructions in language production.},
  language  = {en}
}
@phdthesis{Lange2008,
  author    = {Lange, Dietrich},
  title     = {The South Chilean subduction zone between 41° and 43.5°S : seismicity, structure and state of stress},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-18948},
  school      = {Universit{\"a}t Potsdam},
  year      = {2008},
  abstract  = {Die st{\"a}rksten Erdbeben treten an Subduktionszonen auf, so z.B. das st{\"a}rkste instrumentell jemals gemessene Erdbeben vom 22. Mai 1960 mit einer Magnitude von 9,5 Mw in S{\"u}d Chile. In dieser Arbeit werden lokal gewonnene seismologische Daten aus dem zentralen Bereich des 1960er-Bebens vorgestellt. Das seismologische Netzwerk umfasste den chilenischen Forearc zwischen Tiefseegraben und den vulkanischen Bogen zwischen 41,5°-43,5°S und {\"u}berdeckte sowohl die Insel Chilo{\´e} als auch die Nord-S{\"u}d-streichende Liqui{\~n}e-Ofqui St{\"o}rungszone (LOFZ). Zwischen November 2004 und Oktober 2005 konnten 364 lokale Ereignisse registriert werden. Die gewonnen Aufzeichnungen erlauben Aussagen sowohl {\"u}ber das aktuelle Spannungsfeld im Forearc als auch {\"u}ber das lokale Geschwindigkeitsmodell und die Geometrie der subduzierten Benioff-Zone. Mit einer Auswahl von P- und S-Laufzeiten von gut lokalisierbaren Erdbeben wurden ein Minimum 1-D Geschwindigkeitsmodell, Stationsresiduen und die Hypozentralparameter invertiert. Dieses Geschwindigkeitsmodell diente als Startmodell f{\"u}r die 2-D Tomographie. Das 2-D vp-Modell zeigt eine Zone erh{\"o}hter Geschwindigkeiten unterhalb des L{\"a}ngstals und des {\"o}stlichen Bereiches der Insel Chilo{\´e}, die als Mantelaufw{\"o}lbung interpretiert werden kann. Die Benioff-Zone wird als eine mit ca. 30° ostw{\"a}rts einfallende Struktur abgebildet. Die seismische Hauptaktivit{\"a}t findet parallel zur K{\"u}ste der Insel Chilo{\´e} in Tiefen zwischen 12 und 30 km statt; es handelt sich um Beben, die wahrscheinlich auf der Plattengrenzfl{\"a}che stattfinden. In Tiefen {\"u}ber 70 km l{\"a}sst die Seismizit{\"a}t bereits stark nach, die tiefsten Beben wurden in 120 km Tiefe registriert. Die Abwesenheit tieferer Seismizit{\"a}t wird auf das junge Alter (und eine damit verbundene hohe Temperatur) der ozeanischen Platte zur{\"u}ckgef{\"u}hrt. Neben der Seismizit{\"a}t in der Benioff-Zone treten flache, krustale Beben in verschiedenen H{\"a}ufungen entlang des magmatischen Bogens auf. Diese Bereiche erh{\"o}hter Seismizit{\"a}t sind r{\"a}umlich mit der LOFZ und den Vulkanen Chait{\´e}n, Michinmahuida und Corcovado verkn{\"u}pft. Beben bis zu einer Magnitude von 3,8 Mw zeigen die gegenw{\"a}rtige Aktivit{\"a}t der LOFZ. Herdfl{\"a}chen entlang der LOFZ wurden aus Momententensor-Inversion anhand von Amplitudenspektren von Raumwellen gewonnen. Ergebnisse einer Spannungsfeldinversion zeigen ein Blattverschiebungsregime f{\"u}r den magmatischen Bogen und ein {\"U}berschiebungsregime f{\"u}r Beben in der Benioff-Zone auf. Die hier gemachten seismologischen Beobachtungen, zusammen mit teleseismischen Erdbeben und geologischen Befunden, unterst{\"u}tzen die Modellvorstellung eines sich nordw{\"a}rts bewegenden kontinentalen Forearc-Blocks f{\"u}r S{\"u}d Chile.},
  language  = {en}
}
@phdthesis{Kwiecien2008,
  author    = {Kwiecien, Olga},
  title     = {Paleoenvironmental changes in the Black Sea region during the last 26,000 years : a multi-proxy study of lacustrine sediments from the western Black Sea},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-19180},
  school      = {Universit{\"a}t Potsdam},
  year      = {2008},
  abstract  = {Paleoenvironmental records provide ample information on the Late Quaternary climatic evolution. Due to the great diversity of continental mid-latitude environments the synthetic picture of the past mid-latitudinal climate changes is, however, far from being complete. Owing to its significant size and landlocked setting the Black Sea constitutes a perfect location to study patterns and mechanisms of climate change along the continental interior of Central and Eastern Europe and Asia Minor. Presently, the southern drainage area of the Black Sea is characterized by a Mediterranean-type climate while the northern drainage is under the influence of Central and Northern European climate. During the Last Glacial a decrease in the global sea level disconnected the Black Sea from the Mediterranean Sea transforming it into a giant closed lake. At that time atmospheric precipitation and related with it river run-off were the most important factors driving sediment supply and water chemistry of the Black 'Lake'. Therefore studying properties of the Black Sea sediments provides important information on the interactions and development of the Mediterranean and Central and North European climate in the past. One significant outcome of my thesis is an improved chronostraphigraphical framework for the glacial lacustrine unit of the Black Sea sediment cores, which allowed to refine the environmental history of the Black Sea region and enabled a reliable correlation with data from other marine and terrestrial archives. Data gathered along a N-S transect presented on a common time scale revealed coherent changes in the basin and its surrounding. During the glacial, the southward-shifted Polar Front reduced moisture transport to the northern drainage of the Black Sea and let the southern drainage become dominant in freshwater and sediment supply into the basin. Changes in NW Anatolian precipitation reconstructed from the variability of the terrigenous input imply that during the glacial the regional rainfall variability was strongly influenced by Mediterranean sea surface temperatures and decreased in response to the cooling associated with the North Atlantic Heinrich Events H1 and H2. In contrast to regional precipitation changes, the hydrological properties of the Black Sea remained relatively stable under full glacial conditions. First significant modification in the freshwater/sediment sources reconstructed from changes in the sediment composition, lithology, and 18O of ostracods took place at around 16.4 cal ka BP, simultaneous to the early deglacial northward retreat of the oceanic and atmospheric polar fronts. Meltwater pulses, most probably derived from the disintegrating European ice sheets, changed the isotopic composition of the Black Sea and increased the supply from northern sediment sources. While these changes signalized a mitigation of the Northern European and Mediterranean climate, a decisive increase in local temperature was indicated only later at the transition from the Oldest Dryas to the B{\o}lling around 14.6 cal ka BP. At that time the warming of the Black Sea surface initiated massive phytoplankton blooms, which in turn, induced the precipitation of inorganic carbonates. This biologically triggered process significantly changed the water chemistry and was recorded by simultaneous shifts in the elemental composition of ostracod shells and in the isotopic composition of the inorganically-precipitated carbonates. Starting with the B/A warming and continuing through the YD cold interval and the Early Holocene warming, the Black Sea temperature signal corresponds to the precipitation and temperature changes recorded in the wider Mediterranean region. Early Holocene conditions, similar to those of the B{\o}lling/Aller{\o}d, were punctured by the marine inflow from the Mediterranean at ~ 9.3 cal ka BP, which terminated the lacustrine phase of the Black Sea and had a substantial impact on the chemical and physical properties of its water.},
  language  = {en}
}