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  • 1
    Monograph available for loan
    Monograph available for loan
    Das neue Schuldrecht in der Unternehmenspraxis (2002)
    Köln [u.a.] : Heymanns
    Details Availability
    Call number: M 02.0259/2. Ex.
    Type of Medium: Monograph available for loan
    Pages: 80 S.
    ISBN: 3452251012
    Classification:
    E.1.
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
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    Phenotypic evolution in a fossil gastropod species lineage: evidence for adaptive radiation?
    PANGAEA
    In:  Supplement to: Neubauer, Thomas A; Harzhauser, Mathias; Kroh, A (2013): Phenotypic evolution in a fossil gastropod species lineage: evidence for adaptive radiation? Palaeogeography, Palaeoclimatology, Palaeoecology, 370, 117-126, https://doi.org/10.1016/j.palaeo.2012.11.025
    Details
    Publication Date: 2023-05-12
    Description: Detecting speciation in the fossil record is a particularly challenging matter. Palaeontologists are usually confronted with poor preservation and limited knowledge on the palaeoenvironment. Even in the contrary case of adequate preservation and information, the linkage of pattern to process is often obscured by insufficient temporal resolution. Consequently, reliable documentations of speciation in fossils with discussions on underlying mechanisms are rare. Here we present a well-resolved pattern of morphological evolution in a fossil species lineage of the gastropod Melanopsis in the long-lived Lake Pannon. These developments are related to environmental changes, documented by isotope and stratigraphical data. After a long period of stasis, the ancestral species experiences a phenotypic change expressed as shift and expansion of the morphospace. The appearance of several new phenotypes along with changes in the environment is interpreted as adaptive radiation. Lake-level high stands affect distribution and availability of habitats and, as a result of varied functional demands on shell geometry, the distribution of phenotypes. The on-going divergence of the morphospace into two branches argues for increasing reproductive isolation, consistent with the model of ecological speciation. In the latest phase, however, progressively unstable conditions restrict availability of niches, allowing survival of one branch only.
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 3
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    Measurements of gastropods shell sizes from 23 fossil and extant long-lived lakes (2016)
    PANGAEA
    Details
    Publication Date: 2023-01-13
    Description: Aim: To investigate shell size variation among gastropod faunas of fossil and recent long-lived European lakes and discuss potential underlying processes. Location: 23 long-lived lakes of the Miocene to Recent of Europe. Methods: Based on a dataset of 1412 species of both fossil and extant lacustrine gastropods, we assessed differences in shell size in terms of characteristics of the faunas (species richness, degree of endemism, differences in family composition) and the lakes (surface area, latitude and longitude of lake centroid, distance to closest neighbouring lake) using multiple and linear regression models. Because of a strong species-area relationship, we used resampling to determine whether any observed correlation is driven by that relationship. Results: The regression models indicated size range expansion rather than unidirectional increase or decrease as the dominant pattern of size evolution. The multiple regression models for size range and maximum and minimum size were statistically significant, while the model with mean size was not. Individual contributions and linear regressions indicated species richness and lake surface area as best predictors for size changes. Resampling analysis revealed no significant effects of species richness on the observed patterns. The correlations are comparable across families of different size classes, suggesting a general pattern. Main conclusions: Among the chosen variables, species richness and lake surface area are the most robust predictors of shell size in long-lived lake gastropods. Although the most outstanding and attractive examples for size evolution in lacustrine gastropods derive from lakes with extensive durations, shell size appears to be independent of the duration of the lake as well as longevity of a species. The analogue of long-lived lakes as 'evolutionary islands' does not hold for developments of shell size because different sets of parameters predict size changes.
    Type: Dataset
    Format: application/zip, 134.4 kBytes
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  • 4
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    Tps-files used for the Fast Fourier Analysis
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: Austria; Event label; HAND; HE; Hennersdorf; M, MA; NE; Nexing; NU; Nussdorf; OL; Ollersdorf; Sampling by hand; SG; Siegendorf; St_Margarethen; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 5
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    Boxplots and matrix of Fourier coefficients
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: File content; File name; File size; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 6
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    (Figure 5a) PC1 values for gastropods samples
    PANGAEA
    Details
    Publication Date: 2023-05-12
    Keywords: AGE; Austria; Event label; Factor 1; HAND; HE; Hennersdorf; Latitude of event; Longitude of event; M, MA; NE; Nexing; NU; Nussdorf; OL; Ollersdorf; Sample ID; Sampling by hand; SG; Siegendorf; St_Margarethen
    Type: Dataset
    Format: text/tab-separated-values, 898 data points
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  • 7
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    Morphometric analysis of Melanopsis species (2013)
    PANGAEA
    Details
    Publication Date: 2023-07-10
    Keywords: AGE; Austria; Event label; HAND; HE; Hennersdorf; Latitude of event; Longitude of event; M, MA; Melanopsis coaequata, height; Melanopsis coaequata, width; Melanopsis fossilis, height; Melanopsis fossilis, width; Melanopsis handmanniana, height; Melanopsis handmanniana, width; Melanopsis impressa pseudonarzolina, height; Melanopsis impressa pseudonarzolina, width; Melanopsis rugosa, height; Melanopsis rugosa, width; Melanopsis vindobonensis, height; Melanopsis vindobonensis, width; NE; Nexing; NU; Nussdorf; OL; Ollersdorf; Sample ID; Sampling by hand; SG; Siegendorf; St_Margarethen
    Type: Dataset
    Format: text/tab-separated-values, 2256 data points
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  • 8
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    Friesengeist - Studentisches Medienprojekt zur Internationalen REKLIM Konferenz in Kooperation mit der DEKRA-Hochschule Berlin, Links zum Dokumentarfilm in unterschiedlichen Auflösungen (2014)
    PANGAEA
    In:  Helmholtz-Verbund Regionale Klimaänderungen (REKLIM)
    Details
    Publication Date: 2023-12-06
    Description: Die Menschen in Nordfriesland wissen, dass die Küste – und damit ihre Heimat – kein stabiler Zustand ist, sondern sich ständig verändert. In der Vergangenheit haben mehrfach Sturmfluten das Gesicht der Küste katastrophal verändert. Umso emotionaler ist die Beziehung der Nordfriesen zu ihrer Heimat. Doch auf der Insel Pellworm ist man sich sicher: "Wenn alles weiter seinen jetzigen Gang geht, wird es die Insel in 200 Jahren nicht mehr geben."
    Keywords: File format; File name; File size; Helmholtz-Verbund Regionale Klimaänderungen = Helmholtz Climate Initiative (Regional Climate Change); Pellworm; REKLIM; Uniform resource locator/link to movie; Wadden Sea, North Sea, Germany
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 9
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    Megafauna of the German exploration license area for seafloor massive sulfides along the Central and South East Indian Ridge (Indian Ocean) (2021)
    PANGAEA
    Details
    Publication Date: 2024-03-06
    Description: Background: The growing interest in mineral resources of the deep sea, such as seafloor massive sulfide deposits, has led to an increasing number of exploration licenses issued by the International Seabed Authority. In the Indian Ocean four license areas exist, resulting in an increasing number of new hydrothermal vent fields and the discovery of new species. Most studies focus on active venting areas including their ecology, but the non-vent megafauna of the Central Indian Ridge and South East Indian Ridge remains poorly known. In the framework of the Indian Ocean Exploration project in the German license area for seafloor massive sulfides, baseline imagery and sampling surveys were conducted yearly during research expeditions from 2013 to 2018, using video sledges and Remotely Operated Vehicles. New information: This is the first report of an imagery collection of megafauna from the southern Central Indian- and South East Indian Ridge, reporting the taxonomic richness and their distribution. A total of 218 taxa were recorded and identified based on imagery, with additional morphological and molecular confirmed identifications of 20 taxa from 89 sampled specimens. The compiled fauna catalogue is a synthesis of megafauna occurrences aiming at a consistent morphological identification of taxa and showing their regional distribution. The imagery data was collected during multiple research cruises in different exploration clusters of the German license area, located 500 km north of the Rodriguez Triple Junction along the Central Indian Ridge and 500 km southeast of it along the Southeast Indian Ridge .
    Keywords: 64PE394; 64PE405; 64PE446; Area/locality; Associated Specimens; Behavior; Biodiversity; biodiversity - ecosystem functioning; Camera equipment; Central Indian Ridge; Class; Coordinate uncertainty; Counted; Cruise/expedition; DATE/TIME; Deep-sea mining; DEPTH, water; ELEVATION; Event label; Exposure; Family; fauna catalogue; Focal length; Frame Code; Gear; Genus; Geodetic system; Geographic name/locality; Hydrothermal activity; Hydrothermal vent, age; Hydrothermal vent site, activity; Identification; Identification qualifier; Identification remarks; Image; Image area; Index; INDEX; INDEX2013; INDEX2014; INDEX2014-24VS; INDEX2014-28VS; INDEX2014-31VS; INDEX2014-33VS; INDEX2014-43VS; INDEX2014-44VS; INDEX2014-46VS; INDEX2014-47VS; INDEX2014-49VS; INDEX2014-54VS; INDEX2014-55VS; INDEX2015; INDEX2015-37ROV; INDEX2015-43ROV; INDEX2015-45ROV; INDEX2015-46VS; INDEX2015-47ROV; INDEX2015-48VS; INDEX2015-49ROV; INDEX2015-51ROV; INDEX2015-52VS; INDEX2015-53ROV; INDEX2015-54VS; INDEX2015-56ROV; INDEX2015-58ROV; INDEX2015-59VS; INDEX2015-60ROV; INDEX2015-61VS; INDEX2015-62ROV; INDEX2016; INDEX2016_06ROV; INDEX2016_12ROV; INDEX2016_16ROV; INDEX2016_20ROV; INDEX2016-02ROV; INDEX2017; INDEX2018; INDEX2018-57ROPOS; INDEX2018-59ROPOS; INDEX2018-61ROPOS; INDEX2018-63ROPOS; INDEX2018-65ROPOS; INDEX2018-67ROPOS; INDEX2018-70ROPOS; INDEX2018-71ROPOS; INDEX2018-73ROPOS; INDEX2018-75ROPOS; INDEX2018-80ROPOS; INDEX2018-82ROPOS; INDEX2018-85ROPOS; INDEX2018-95ROPOS; INDEX2018-97ROPOS; INDEX2018-99ROPOS; Indian Ocean; Institution; ISO-speed; Kingdom; Language; LATITUDE; Leg Number; Life stage; LONGITUDE; Marine polymetallic sulphides (INDEX) – Germany's exploration license in the Indian Ocean; Marker; Method comment; Name; Number of individuals; Occurrence; Ocean Floor Observation System; OFOS; Order; PCR result; Pelagia; Photograph frame code; photographs; Phylum; Pourquoi Pas ? (2005); Remote operated platform for oceanography; Remote operated vehicle; Rodriguez Triple Junction; ROPOS; ROV; Salinity; Sample area/volume; Sampled; Sample ID; Scientific Name authorship; Sequence result; SO230-17-1; SO230-28-1; SO230-31-1; SO230-35-1; SO230-36-1; SO230-38-1; SO230-39-1; SO230-47-1; SO230-49-1; SO230-51-1; SO230-55-1; SO230-57-1; SO230-59-1; SO230-62-1; SO259; SO259_74-1; SO259_83-1; SO259_86-1; SO259_94-1; SOIndex2013; SOIndex2013_17-1; SOIndex2013_28-1; SOIndex2013_31-1; SOIndex2013_35-1; SOIndex2013_36-1; SOIndex2013_38-1; SOIndex2013_39-1; SOIndex2013_44-1; SOIndex2013_47-1; SOIndex2013_49-1; SOIndex2013_51-1; SOIndex2013_55-1; SOIndex2013_57-1; SOIndex2013_59-1; SOIndex2013_62-1; Sonne; Sonne_2; South East Indian Ridge; Species identification; Station label; Taxonomist; Taxon rank; Temperature, water; Tissue Descriptor; Transect; Type; Underwater Video system; Use; UWV; Vessel; VICTOR; Victor6000 ROV; Video/photo sled ID code; video imagery; Video sled; VIDS; Voucher Specimen Code; Water Body; Year of observation
    Type: Dataset
    Format: text/tab-separated-values, 106499 data points
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  • 10
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    Oligocene-Miocene basin evolution in SE Anatolia, Turkey: constraints on the closure of the eastern Tethys gateway (2009)
    In:  Geological Society Special Publication 311: 107-132.
    Details
    Publication Date: 2009-04-30
    Description: The Oligocene-Miocene was a time characterized by major climate changes as well as changing plate configurations. The Middle Miocene Climate Transition (17 to 11 Ma) may even have been triggered by a plate tectonic event: the closure of the eastern Tethys gateway, the marine connection between the Mediterranean and Indian Ocean. To address this idea, we focus on the evolution of Oligocene and Miocene foreland basins in the southernmost part of Turkey, the most likely candidates to have formed this gateway. In addition, we take the geodynamic evolution of the Arabian-Eurasian collision into account. The Mu[s] and Elaz[i][g] basins, located to the north of the Bitlis-Zagros suture zone, were most likely connected during the Oligocene. The deepening of both basins is biostratigraphically dated by us to occur during the Rupelian (Early Oligocene). Deep marine conditions (between 350 and 750 m) prevailed until the Chattian (Late Oligocene), when the basins shoaled rapidly to subtidal/intertidal environment in tropical to subtropical conditions, as indicated by the macrofossil assemblages. We conclude that the emergence of this basin during the Chattian severely restricted the marine connection between an eastern (Indian Ocean) and western (Mediterranean) marine domain. If a connection persisted it was likely located south of the Bitlis-Zagros suture zone. The Kahramanmara[s] basin, located on the northern Arabian promontory south of the Bitlis-Zagros suture zone, was a foreland basin during the Middle and Late Miocene, possibly linked to the Hatay basin to the west and the Lice basin to the east. Our data indicates that this foreland basin experienced shallow marine conditions during the Langhian, followed by a rapid deepening during Langhian/Serravallian and prevailing deep marine conditions (between 350 and 750 m) until the early Tortonian. We have dated the youngest sediments underneath a subduction-related thrust at c. 11 Ma and suggest that this corresponds to the end of underthrusting in the Kahramanmara[s] region, i.e. the end of subduction of Arabia. This age coincides in time with the onset of eastern Anatolian volcanism, uplift of the East Anatolian Accretionary Complex, and the onset of the North and East Anatolian Fault Zones accommodating westward escape tectonics of Anatolia. After c. 11 Ma, the foreland basin south of the Bitlis formed not (or no longer) a deep marine connection along the northern margin of Arabia between the Mediterranean Sea and the Indian Ocean. We finally conclude that a causal link between gateway closure and global climate change to a cooler mode, recorded in the Mi3b event ({delta}18O increase) dated at 13.82 Ma, cannot be supported.
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