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  • 03. Hydrosphere::03.04. Chemical and biological::03.04.05. Gases  (1)
  • Decapodiformes/anatomy & histology/*chemistry  (1)
  • 2020-2023
  • 2020-2022
  • 2005-2009  (2)
  • 1930-1934
  • 1
    Publication Date: 2008-03-29
    Description: The beak of the Humboldt squid Dosidicus gigas represents one of the hardest and stiffest wholly organic materials known. As it is deeply embedded within the soft buccal envelope, the manner in which impact forces are transmitted between beak and envelope is a matter of considerable scientific interest. Here, we show that the hydrated beak exhibits a large stiffness gradient, spanning two orders of magnitude from the tip to the base. This gradient is correlated with a chemical gradient involving mixtures of chitin, water, and His-rich proteins that contain 3,4-dihydroxyphenyl-L-alanine (dopa) and undergo extensive stabilization by histidyl-dopa cross-link formation. These findings may serve as a foundation for identifying design principles for attaching mechanically mismatched materials in engineering and biological applications.〈br /〉〈br /〉〈a href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC2754134/" target="_blank"〉〈img src="https://static.pubmed.gov/portal/portal3rc.fcgi/4089621/img/3977009" border="0"〉〈/a〉   〈a href="https://www.ncbi.nlm.nih.gov/pmc/articles/PMC2754134/" target="_blank"〉This paper as free author manuscript - peer-reviewed and accepted for publication〈/a〉〈br /〉〈br /〉〈span class="detail_caption"〉Notes: 〈/span〉Miserez, Ali -- Schneberk, Todd -- Sun, Chengjun -- Zok, Frank W -- Waite, J Herbert -- DE015415/DE/NIDCR NIH HHS/ -- R01 DE014672/DE/NIDCR NIH HHS/ -- R01 DE015415/DE/NIDCR NIH HHS/ -- R01 DE015415-01/DE/NIDCR NIH HHS/ -- R01 DE015415-03/DE/NIDCR NIH HHS/ -- R01 DE015415-04/DE/NIDCR NIH HHS/ -- New York, N.Y. -- Science. 2008 Mar 28;319(5871):1816-9. doi: 10.1126/science.1154117.〈br /〉〈span class="detail_caption"〉Author address: 〈/span〉Materials Department, University of California, Santa Barbara, CA 93106, USA.〈br /〉〈span class="detail_caption"〉Record origin:〈/span〉 〈a href="http://www.ncbi.nlm.nih.gov/pubmed/18369144" target="_blank"〉PubMed〈/a〉
    Keywords: Amino Acids/analysis ; Animals ; Beak/anatomy & histology/*chemistry ; Biomechanical Phenomena ; Chitin/*analysis/chemistry ; Compliance ; Decapodiformes/anatomy & histology/*chemistry ; Dihydroxyphenylalanine/analysis/*chemistry ; Dopamine/analogs & derivatives/analysis ; Freeze Drying ; Glucosamine/analysis ; Hardness ; Histidine/analysis/chemistry ; Pigmentation ; Proteins/*analysis/chemistry ; Water/*analysis
    Print ISSN: 0036-8075
    Electronic ISSN: 1095-9203
    Topics: Biology , Chemistry and Pharmacology , Computer Science , Medicine , Natural Sciences in General , Physics
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  • 2
    Publication Date: 2022-02-16
    Description: The assessment of gas origin in mud volcanoes and related petroleum systems must consider postgenetic processes which may alter the original molecular and isotopic composition of reservoir gas. Beyond eventual molecular and isotopic fractionation due to gas migration and microbial oxidation, investigated in previous studies, we now demonstrate that mud volcanoes can show signals of anaerobic biodegradation of natural gas and oil in the subsurface. A large set of gas geochemical data from more than 150 terrestrial mud volcanoes worldwide has been examined. Due to the very low amount of C2+ in mud volcanoes, isotopic ratios of ethane, propane and butane (generally the best tracers of anaerobic biodegradation) are only available in a few cases. However, it is observed that 13C-enriched propane is always associated with positive б13 CCO2 values, which are known indicators of secondary methanogenesis following anaerobic biodegradation of petroleum. Data from carbon isotopic ratio of CO2 are available for 134 onshore mud volcanoes from 9 countries (Azerbaijan, Georgia, Ukraine, Russia, Turkmenistan, Trinidad, Italy, Japan and Taiwan). Exactly 50% of mud volcanoes, all releasing thermogenic or mixed methane, show at least one sample with б13 CCO2〉+5‰ (PDB). Thermogenic CH4 associated with positive carbon isotopic ratio of CO2 generally maintains its б13C-enriched signature, which is therefore not perturbed by the lighter secondary microbial gas. There is, however, high variability in the б13 CCO2 values within the same mud volcanoes, so that positive б13 CCO2 values can be found in some vents and not in others, or not continuously in the same vent. This can be due to high sensitivity of б13 CCO2 to gas–water–rock interactions or to the presence of differently biodegraded seepage systems in the same mud volcano. However, finding a positive б13 CCO2 value should be considered highly indicative of anaerobic biodegradation and further analyses should be made, especially if mud volcanoes are to be used as pathfinders of the conditions indicative of subsurface hydrocarbon accumulations in unexplored areas.
    Description: Published
    Description: 1692-1703
    Description: 4.5. Studi sul degassamento naturale e sui gas petroliferi
    Description: JCR Journal
    Description: reserved
    Keywords: Mud volcanoes ; Methane ; Secondary methanogenesis ; Anaerobic biodegradation ; Isotopically enriched CO2 ; 03. Hydrosphere::03.04. Chemical and biological::03.04.05. Gases
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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