@phdthesis{Archuby2009, author = {Archuby, Fernando}, title = {Taphonomy and palaeoecology of benthic macroinvertebrates from the Agua de la Mula Member of the Agrio Formation, Neuqu{\´e}n Basin (Neuqu{\´e}n province, Argentina): sequence stratigraphic significance}, url = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-37177}, school = {Universit{\"a}t W{\"u}rzburg}, year = {2009}, abstract = {The taphonomic and paleoecologic aspects of the Upper Hauterivian to Lower Barremian Agua de la Mula Member of the Agrio Formation (Neuqu{\´e}n Basin, Argentina) were studied in the frame of the sequence stratigraphic paradigm. The Agua de la Mula Member, a ca. 600 m thick succession of highly cyclic marine sediments was surveyed at two localities. Detailed bed-by-bed sedimentologic, stratigraphic, ichnologic, taphonomic and paleoecologic data collection allowed a precise paleoenvironmental, stratigraphic, taphonomic and synecologic interpretation, in a controlled sequence stratigraphic framework. The main architectural stratigraphic component is the Starvation-Dilution Sequence, interpreted as a the effect of a sixth-order, Milankovitch precession-driven cycle. Dilution hemisequences are siliciclastic-dominated and show evidence of depth changes. Starvation hemisequences show a diverse variation of mixed carbonate-siliciclastic facies that is linked to sequence stratigraphy. Ammonite-based biostratigraphy was revised and new knowledge proposed. The stratigraphic framework was improved by combining biostratigraphy, sequence stratigraphy and event stratigraphy. Nine main sequences were described, linked to other stratigraphic markers and correlated with other sequence stratigraphic charts. Several orders of cyclicity were inferred. Third- and fourth-order sequences are the major sequences, not subordinated to higher hierarchies (lower order). Precession, obliquity, and short and long eccentricity cycles of the Milankovitch band are proposed. Among the different sequence stratigraphic models the transgression-regression model fits the majority of the sequences described in this work. The depositional-sequence model could be applied only to the first third-order sequence, in which the true sequence boundary is identifiable. Starvation-dilution sequences, however, are composed by to components that are not completely explained by those models. Starvation hemisequences developed in intermediate to deep settings record the transgressive phase as well as the earLy regressive one without visible stratigraphic boundaries. 112 samples with 22,572 individuals were grouped into fifteen fossil associations and one assemblage that reflect the interaction of different factors: age, position in major, medium and starvation dilution sequences and, linked to sequence stratigraphy, depth, oxygen availability, rate of terrigenous input, water agitation, and substrate conditions. Temporary possible reduction in oxygen content is inferred based on all sources of available evidence. Organic buildups are briefly described and their development interpreted in terms of the sequence stratigraphic framework. Vertical patterns of replacement of fossil associations are described and related to sequence stratigraphy. Five types of skeletal concentrations represent the diversity of coquinas decribed in this study. Type 1, 2, 4 and 5 correspond to starvation hemisequences deposited in progressively shallower settings, from basin to inner ramp. Type 3 is embedded into dilution hemisequences and inferred to be linked to shell bed type I of Kidwell (1985). Types 1 and 2 correspond to transgression, maximum flooding and early regression without distinction. Type 4A as well as Type 5 are interpreted as onlap shell beds (Kidwell 1991a) or early TST shell beds (F{\"u}rsich and Pandey 2003). Type 4B corresponds to the MFZ shell bed (F{\"u}rsich and Pandey 2003) or mid-cycle shell bed (Abbott 1997), while Type 4C to the downlap shell bed (Kidwell 1991a). Time-averaging of shell beds was assessed with precision as the time involved in the deposition of the starvation hemisequences could be inferred. All shell beds comprise within-habitat assemblages forming within a few thousand years, with little environmental condensation. The fossilization of the marine calcareous shells is modelled as a series of steps called windows: environmental, destructional, burial and diagenetic. The "diagenetic window" is the most relevant. Connected to this it is proposed that carbonate dissolution is the primary control on the development of shell beds, as has been proposed before (F{\"u}rsich 1982; F{\"u}rsich and Pandey 2003). The interpretative power resulting from combining several lines of evidence, e.g., facies analysis, sequence stratigraphy, biostratigraphy, trace fossil analysis, paleoecology and taphonomy, and unravelling their multiple relationships, are the most relevant conclusions of this study.}, subject = {W{\"u}rzburg / Institut f{\"u}r Pal{\"a}ontologie}, language = {en} } @phdthesis{Tomašovych2006, author = {Tomašov{\´y}ch, Adam}, title = {Differential effects of environmental factors on ecology of brachiopods and bivalves during the Late Triassic and Jurassic}, url = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-19131}, school = {Universit{\"a}t W{\"u}rzburg}, year = {2006}, abstract = {The aim of this study was to assess distribution patterns of articulate brachiopods during the Mesozoic. Exploratory and confirmatory multivariate analyses in this study evaluate whether environmental preferences of brachiopods and bivalves are substantially distinct and whether structure of their communities significantly differ. Specifically, the hypothesis being tested is that differential abundances of Mesozoic brachiopods and bivalves are not related to varying substrate properties only, but also to varying food supply, turbidity and oxygen levels. This hypothesis was evaluated with quantitative data gathered in various field areas and time intervals. They include the Upper Triassic deposits of the West Carpathians and Eastern Alps, the Lower and Middle Jurassic deposits of Morocco, the Middle and Upper Jurassic deposits of the West Carpathians, the Upper Jurassic deposits of the Franconian and Swabian Alb, and the Upper Jurassic deposits of the Swiss Jura. The main conclusion is that brachiopod-dominated communities are characterized by a unique guild structure, with dominance of trophic groups with low metabolic requirements or adapted to nutrient-poor or oxygen-poor conditions. For example, brachiopod co-occured more commonly with epifaunal than with infaunal bivalves in soft-bottom environments. Abundances of brachiopods correlate mostly negatively with increasing proportions of terrigenous admixture (i.e., with increasing amount of land-derived nutrient supply and turbidity).}, subject = {Fossile Armf{\"u}ßer}, language = {en} } @article{HornickRichterHarpoleetal.2022, author = {Hornick, Thomas and Richter, Anett and Harpole, William Stanley and Bastl, Maximilian and Bohlmann, Stephanie and Bonn, Aletta and Bumberger, Jan and Dietrich, Peter and Gemeinholzer, Birgit and Grote, R{\"u}diger and Heinold, Bernd and Keller, Alexander and Luttkus, Marie L. and M{\"a}der, Patrick and Motivans Švara, Elena and Passonneau, Sarah and Punyasena, Surangi W. and Rakosy, Demetra and Richter, Ronny and Sickel, Wiebke and Steffan-Dewenter, Ingolf and Theodorou, Panagiotis and Treudler, Regina and Werchan, Barbora and Werchan, Matthias and Wolke, Ralf and Dunker, Susanne}, title = {An integrative environmental pollen diversity assessment and its importance for the Sustainable Development Goals}, series = {Plants, People, Planet}, volume = {4}, journal = {Plants, People, Planet}, number = {2}, doi = {10.1002/ppp3.10234}, url = {http://nbn-resolving.de/urn:nbn:de:bvb:20-opus-276487}, pages = {110 -- 121}, year = {2022}, abstract = {Societal Impact Statement Pollen relates to many aspects of human and environmental health, which protection and improvement are endorsed by the United Nations Sustainable Development Goals. By highlighting these connections in the frame of current challenges in monitoring and research, we discuss the need of more integrative and multidisciplinary pollen research related to societal needs, improving health of humans and our ecosystems for a sustainable future. Summary Pollen is at once intimately part of the reproductive cycle of seed plants and simultaneously highly relevant for the environment (pollinators, vector for nutrients, or organisms), people (food safety and health), and climate (cloud condensation nuclei and climate reconstruction). We provide an interdisciplinary perspective on the many and connected roles of pollen to foster a better integration of the currently disparate fields of pollen research, which would benefit from the sharing of general knowledge, technical advancements, or data processing solutions. We propose a more interdisciplinary and holistic research approach that encompasses total environmental pollen diversity (ePD) (wind and animal and occasionally water distributed pollen) at multiple levels of diversity (genotypic, phenotypic, physiological, chemical, and functional) across space and time. This interdisciplinary approach holds the potential to contribute to pressing human issues, including addressing United Nations Sustainable Development Goals, fostering social and political awareness of these tiny yet important and fascinating particles.}, language = {en} }