Endogenous synchronization of the chemical signature of Reticulitermes (Isoptera: Rhinotermitidae) worker termites

2011 ◽  
Vol 47 (1-2) ◽  
pp. 202-208 ◽  
Author(s):  
Anne-Geneviève Bagnères ◽  
Eric Darrouzet ◽  
Xavier Landré ◽  
Jean-Philippe Christidès
Keyword(s):  
2018 ◽  
Author(s):  
Koen Vercruysse ◽  
Margaret M. Whalen

<p>This report is a continuation of previous research on the H<sub>2</sub>O<sub>2</sub>-mediated synthesis of melanin-like pigments. We synthesized and characterized L-DOPA-based pigments using air- or H<sub>2</sub>O<sub>2</sub>-mediated<sub> </sub>oxidation. We compared their physic-chemical properties and evaluated their capacity to affect the interleukin release from immune cells. The use of higher concentrations of H<sub>2</sub>O<sub>2</sub> resulted in melanin-like materials with a distinct chemical signature in their FT-IR spectra and a lighter color. All pigments enhanced the interleukin release from immune cells. The possibility that lighter-colored melanins can be generated is discussed in the context of the importance of melanin-based pigmentation in human physiology.</p>


2016 ◽  
Vol 155 (3) ◽  
pp. 568-585 ◽  
Author(s):  
JOHN N. HOOKER ◽  
JOE CARTWRIGHT

AbstractA long-debated aspect of cone-in-cone structures is whether the mineral aggregates composing the structure precipitated with their conical form (primary cone-in-cone), or whether the cones formed after precipitation (secondary cone-in-cone). A calcite deposit from the Cretaceous of Jordan bears all the defining characteristics of the structure. Trace dolomite within the sample supports the primary cone-in-cone hypothesis. The host sediment is a biosiliceous mudstone containing abundant rhombohedral dolomite grains. Dolomite rhombohedra are also distributed throughout the calcite of the cone-in-cone. The rhombohedra within the calcite locally have dolomite overgrowths that are aligned with calcite fibres. Evidence that dolomite co-precipitated with calcite, and did not replace calcite, includes (i) preferential downward extension of dolomite overgrowths, in the presumed growth-direction of the cone-in-cone, from the dolomite grains on which they nucleate, and (ii) planar, vertical borders between dolomite crystals and calcite fibres. Because dolomite overgrows host-sediment rhombohedra and forms part of the cones, it follows that the host-sediment was incorporated into the growing cone-in-cone as the calcite precipitated, and not afterward. The host-sediment was not injected into the cone-in-cone along fractures, as the secondary-origin theory suggests. This finding implies that cone-in-cone in general does not form over multiple stages, and thus has greater potential to preserve the chemical signature of its original precipitation.


Chemoecology ◽  
2021 ◽  
Author(s):  
Denise Sguarizi-Antonio ◽  
Kamylla Balbuena Michelutti ◽  
Eva Ramona Pereira Soares ◽  
Nathan Rodrigues Batista ◽  
Sidnei Eduardo Lima-Junior ◽  
...  

2022 ◽  
Author(s):  
Li Su ◽  
Fengjiao Zhao ◽  
Huahang Yu ◽  
Min Bai ◽  
Jing Xue ◽  
...  

Both sequence enrichment and base resolution is essential for accurate sequencing analysis of low-abundance RNA. Yet it is hindered by the lack of molecular tools. Here we report a bifunctional...


2021 ◽  
Author(s):  
Srisuda Rojsatien ◽  
Trumann Walker ◽  
Tara Nietzold ◽  
Barry Lai ◽  
Eric Colegrove ◽  
...  
Keyword(s):  

2020 ◽  
Vol 635 ◽  
pp. A8 ◽  
Author(s):  
L. Casamiquela ◽  
Y. Tarricq ◽  
C. Soubiran ◽  
S. Blanco-Cuaresma ◽  
P. Jofré ◽  
...  

Context. Well studied open clusters (OCs) of the solar neighborhood are frequently used as reference objects to test galactic and stellar theories. For that purpose, their chemical composition needs to be known with a high level of confidence. It is also important to clarify if each OC is chemically homogeneous and if it has a unique chemical signature. Aims. The aims of this work are (1) to determine accurate and precise abundances of 22 chemical species (from Na to Eu) in the Hyades, Praesepe, and Rupecht 147 by using a large number of stars at different evolutionary states, (2) to evaluate the level of chemical homogeneity of these OCs, and (3) to compare their chemical signatures. Methods. We gathered ∼800 high resolution and high signal-to-noise spectra of ∼100 members in the three clusters, which were obtained with the latest memberships based on Gaia DR2 data. We built a pipeline, which computes atmospheric parameters and strictly line-by-line differential abundances among twin stars in our sample. With this method, we were able to reach a very high precision in the abundances (0.01–0.02 dex in most of the elements). Results. We find large differences in the absolute abundances in some elements, which can be attributed to diffusion, non-local thermodynamic equilibrium (non-LTE) effects, or systematics in the analysis. For the three OCs, we find strong correlations in the differential abundances between different pairs of elements. According to our experiment with synthetic data, this can be explained by some level of chemical inhomogeneity. We compare differential abundances of several stars from the Hyades and Praesepe tails: The stars that differ more in chemical abundances also have distinct kinematics, even though they have been identified as members of the tail. Conclusions. It is possible to obtain high precision abundances using a differential analysis even when mixing spectra from different instruments. With this technique, we find that the Hyades and Preasepe have the same chemical signature when G dwarfs and K giants are considered. Despite a certain level of inhomogeneity in each cluster, it is still possible to clearly distinguish the chemical signature of the older cluster Ruprecht 147 when compared to the Hyades and Praesepe.


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