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  • 1
    Electronic Resource
    Electronic Resource
    Induction of maleate hydratase in Pseudomonas pseudoalcaligenes (1997)
    Springer
    World journal of microbiology and biotechnology 13 (1997), S. 279-282 
    Details
    ISSN: 1573-0972
    Keywords: d-malate ; enzyme induction ; malease ; maleate hydratase ; Pseudomonas pseudoalcaligenes
    Source: Springer Online Journal Archives 1860-2000
    Topics: Biology , Process Engineering, Biotechnology, Nutrition Technology
    Notes: Abstract Maleate hydratase (malease, EC 4.2.1.31) activity in P. pseudoalcaligenes is induced when grown on3-hydroxybenzoate. The specific malease activity was constant during the logarithmic phase in a batch culture containing 3-hydroxybenzoate as the carbon source, when 3-hydroxybenzoate-grown cells were used as inoculum. When yeast extract-grown cells were used as inoculum, the specific malease activity was correlated with growth. In both instances the specific malease activity dropped rapidly as soon as growth ceased. Maleate did not serve as a growth substrate for this microorganism, but a mutant able to grow on maleate was selected. The specific malease activity of maleate-grown cells of this mutant was not higher than the basal level of induction of malease activity.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1023/A:1018526822535
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    Paper (German National Licenses)
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  • 2
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    A detection of Milankovitch frequencies in tephra records of arc volcanism (2013)
    In:  [Invited talk] In: AGU Fall Meeting 2013, 07.-13.12.2013, San Francisco, USA .
    Details
    Publication Date: 2019-09-23
    Type: Conference or Workshop Item , NonPeerReviewed
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    OceanRep: Talk
  • 3
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    A detection of Milankovitch Periodocity in records of global arc volcanism (2010)
    In:  [Poster] In: AGU Fall Meeting 2010, 13.12.-17.12.2010, San Francisco, California, USA .
    Details
    Publication Date: 2012-02-23
    Description: PP31C-1638 The intervals between volcanic activity varies on a wide range of spatial and temporal scales, from less than a year in single volcanic systems to timescales of 10^6 years and longer in global volcanism. The causes of these timescales are poorly understood although the long-term global variations are likely linked to plate-tectonic processes. Here we present evidence for temporal changes in eruption frequencies at an intermediate timescale (10 000 years). In particular we use the Pleistocene to Recent records of widespread tephras of sub-Plinian to Plinian, and occasionally co-ignimbrite origin, along the Pacific Ring of Fire, which accounts for about half of the global length of 44,000 km of active subduction. Eruptions at arc volcanoes tend to be highly explosive and the well-preserved tephra records from the ocean floor can be assumed to be representative of how eruption frequencies varied with time. We show that volcanic activity along the Pacific Ring of Fire evolved through alternating intervals of high and low activity; although there are regional differences, these variations in activity have a statistically significant periodicity of approximately 41 ka that matches the temporal variation in the Earth's obliquity. This suggests that the timescale of volcanic activity is controlled by effects of global climate changes which result in redistribution of water masses between oceans and polar ice caps. While our statistical correlations suggest that the timescale of volcanic activity is controlled by effects of global climate changes, the physical nature of these effects is presently investigated.
    Type: Conference or Workshop Item , NonPeerReviewed
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    OceanRep: Poster
  • 4
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    A statistical analysis of the correlation between large igneous provinces and lower mantle seismic structure (2014)
    Oxford University Press
    Details
    Publication Date: 2014-03-21
    Description: Large igneous provinces (LIPs) lie approximately above the margins of the African and Pacific large low shear velocity provinces (LLSVPs) in the deep mantle. This spatial correlation has been used to argue that plumes are preferentially generated at the margins of LLSVPs. We perform a series of Monte Carlo–based statistical tests to assess the uniqueness of this conclusion. These tests indicate that (1) the reconstructed locations of LIPs are significantly correlated with both slower-than-average shear wave velocity regions, which contain LLSVPs, and the margins of these structures; and (2) these correlations cannot be statistically distinguished. That is, given current constraints, if plumes were generated randomly throughout regions of slower-than-average shear wave velocity in the deep mantle, then statistical tests are expected to show a significant correlation between the locations of LIPs and the margins of LLSVPs. We therefore conclude that it is premature to argue that the margins of LLSVPs represent preferred zones of plume generation. This conclusion is reinforced in our analysis by a demonstration that the expected mean distance of a set of points randomly placed in slower-than-average shear wave velocity regions is consistent with the observed mean distance between LIPs and the margins of LLSVPs. Finally, we also test the correlation between the reconstructed locations of LIPs and the horizontal gradient in deep mantle shear velocity perturbations. We find, given the uncertainty implied by different tomography models, that there is no statistically significant correlation and that being in a slow region (i.e. in the region of LLSVPs) is a stronger geographic requirement for plume generation than being at a specific (high) gradient.
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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  • 5
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    Detection of a dynamic topography signal in last interglacial sea-level records (2017)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 2017-07-08
    Description: Estimating minimum ice volume during the last interglacial based on local sea-level indicators requires that these indicators are corrected for processes that alter local sea level relative to the global average. Although glacial isostatic adjustment is generally accounted for, global scale dynamic changes in topography driven by convective mantle flow are generally not considered. We use numerical models of mantle flow to quantify vertical deflections caused by dynamic topography and compare predictions at passive margins to a globally distributed set of last interglacial sea-level markers. The deflections predicted as a result of dynamic topography are significantly correlated with marker elevations (〉95% probability) and are consistent with construction and preservation attributes across marker types. We conclude that a dynamic topography signal is present in the elevation of last interglacial sea-level records and that the signal must be accounted for in any effort to determine peak global mean sea level during the last interglacial to within an accuracy of several meters.
    Electronic ISSN: 2375-2548
    Topics: Natural Sciences in General
    Published by American Association for the Advancement of Science (AAAS)
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  • 6
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    A 65 k.y. time series from sediment-hosted glasses reveals rapid transitions in ocean ridge magmas (2017)
    Geological Society of America (GSA)
    In: Geology
    Details
    Publication Date: 2017-05-13
    Description: Studies of ocean ridge magmatism have been hampered by the difficulty in constructing time-series data over more than a few thousand years. Sediment rapidly covers newly formed ocean crust, and older rocks, even when recovered from fault scarps, cannot be dated accurately. Ridge eruptions, however, disperse pyroclastic glass over distances as far as 5 km, and these glasses have been shown to persist for thousands of years in on-ridge sediment push cores. Here we present data on such glasses from a piston core that impacted basement in much older (600 ka) sediment. The age of deposition was determined using established stratigraphic methods to date the host sediment, yielding an average sample resolution of a few thousand years and a continuous 65 k.y. time series. The new time-series data show systematic temporal variations in magma compositions related to a change to the dynamics of crustal storage, which led to greater extents of pre-eruptive differentiation. Shortly thereafter was a small but discernable shift toward more enriched primary melt compositions. These events coincide with the onset of enhanced crustal production, previously identified using seismic data and interpreted to reflect the capture of a hotspot by the ridge. These results show the long-term preservation of pyroclastic glasses and suggest that the construction of high-resolution volcanic stratigraphy over a million years or more may be possible at ocean ridges, using multiple piston cores that impact basement. Sediment-hosted glasses have the potential to transform ocean ridges from the volcanic setting with the worst time-series data to that with the best.
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
    Published by Geological Society of America (GSA)
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  • 7
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    Slow climate mode reconciles historical and model-based estimates of climate sensitivity (2017)
    American Association for the Advancement of Science (AAAS)
    Details
    Publication Date: 2017-07-06
    Description: The latest Intergovernmental Panel on Climate Change Assessment Report widened the equilibrium climate sensitivity (ECS) range from 2° to 4.5°C to an updated range of 1.5° to 4.5°C in order to account for the lack of consensus between estimates based on models and historical observations. The historical ECS estimates range from 1.5° to 3°C and are derived assuming a linear radiative response to warming. A Bayesian methodology applied to 24 models, however, documents curvature in the radiative response to warming from an evolving contribution of interannual to centennial modes of radiative response. Centennial modes display stronger amplifying feedbacks and ultimately contribute 28 to 68% (90% credible interval) of equilibrium warming, yet they comprise only 1 to 7% of current warming. Accounting for these unresolved centennial contributions brings historical records into agreement with model-derived ECS estimates.
    Electronic ISSN: 2375-2548
    Topics: Natural Sciences in General
    Published by American Association for the Advancement of Science (AAAS)
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  • 8
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    Temperature extremes: Changing mean, not variance [Physical Sciences] (2013)
    National Academy of Sciences
    Details
    Publication Date: 2013-02-13
    Description: Hansen et al. (1) demonstrated that the probability of extremely hot summers has markedly increased because the mean of the distribution of seasonally averaged temperatures has increased. However, the authors also implied that the variance of the distribution has increased, a result that differs from regional studies that show changes...
    Keywords: Letters
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
    Published by National Academy of Sciences
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  • 9
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    SST variability beyond decadal timescales [Earth, Atmospheric, and Planetary Sciences] (2014)
    National Academy of Sciences
    Details
    Publication Date: 2014-11-26
    Description: The variability of sea surface temperatures (SSTs) at multidecadal and longer timescales is poorly constrained, primarily because instrumental records are short and proxy records are noisy. Through applying a new noise filtering technique to a global network of late Holocene SST proxies, we estimate SST variability between annual and millennial...
    Print ISSN: 0027-8424
    Electronic ISSN: 1091-6490
    Topics: Biology , Medicine , Natural Sciences in General
    Published by National Academy of Sciences
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  • 10
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    A detection of Milankovitch frequencies in global volcanic activity (2013)
    Geological Society of America (GSA)
    In: Geology
    Details
    Publication Date: 2013-01-30
    Description: A rigorous detection of Milankovitch periodicities in volcanic output across the Pleistocene-Holocene ice age has remained elusive. We report on a spectral analysis of a large number of well-preserved ash plume deposits recorded in marine sediments along the Pacific Ring of Fire. Our analysis yields a statistically significant detection of a spectral peak at the obliquity period. We propose that this variability in volcanic activity results from crustal stress changes associated with ice age mass redistribution. In particular, increased volcanism lags behind the highest rate of increasing eustatic sea level (decreasing global ice volume) by 4.0 ± 3.6 k.y. and correlates with numerical predictions of stress changes at volcanically active sites. These results support the presence of a causal link between variations in ice age climate, continental stress field, and volcanism.
    Print ISSN: 0091-7613
    Electronic ISSN: 1943-2682
    Topics: Geosciences
    Published by Geological Society of America (GSA)
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