Results 31 to 40 of about 1,653,801 (181)

Divergent trajectories of genome architecture and chromosome evolution in ferns and angiosperms

open access: yesNew Phytologist, Volume 252, Issue 1, Page 427-442, October 2026.
Variation in key fern genomic traits across families, mapped onto a summary phylogenetic tree. Summary Ferns and angiosperms represent the two largest vascular plant lineages but exhibit striking genomic and ecological contrasts. We investigated whether differences in genome size, chromosome architecture, GC content, and stomatal traits reveal ...
Petr Bureš   +14 more
wiley   +1 more source

In eigener Sache [PDF]

open access: yes, 2023
Liebe Leser*innen von ACT, diese Ausgabe von ACT beginnt mit einem wichtigen Hinweis in eigener Sache. Das Forschungsinstitut für Musiktheater der Universität Bayreuth auf Schloß Thurnau (fimt) hat eine schon lange Geschichte, die ins Jahr 1976 ...
Mungen, Anno
core  

Coexistence of stable branched patterns in anisotropic inhomogeneous systems

open access: yesNew Journal of Physics, 2015
A new class of pattern forming systems is identified and investigated: anisotropic systems that are spatially inhomogeneous along the direction perpendicular to the preferred one.
B Kaoui   +4 more
doaj   +1 more source

Crystal structure of (2,6-diisopropyl-phenyl)-[6-(2,6-dimethyl-phenyl)- pyridin-2-yl-methylene]-aminopalladium(II) dichloromethane trisolvate, Pd(C26H30N2)Cl2 · 3CH2Cl2

open access: yesZeitschrift für Kristallographie - New Crystal Structures, 2005
C29H36Cl8N2Pd, orthorhombic, P212121 (no. 19), a = 16.5460(8) Å, b = 17.995(1) Å, c = 11.817(1) Å, V = 3518.5 Å3, Z = 4, Rgt(F) = 0.037, wRref(F2) = 0.099, T = 193 K.
Maisel H.   +3 more
doaj   +1 more source

Crystal structure of N,N′-bis(2-methyl-4,5-diphenylimidazo[ 1,5-b]pyridazin-7-yl)-1,3-diaminopropane ethanol solvate, C3H6(NH)2(C19H14N3)2 · C2H5OH

open access: yesZeitschrift für Kristallographie - New Crystal Structures, 2006
C43H42N8O, triclinic, P1̅ (no. 2), a = 9.997(2) Å, b = 12.046(2) Å, c = 15.635(3) Å, α = 90.84(3)°, β = 105.18(3)°, γ = 93.43(3)°, V = 1813.0 Å3, Z = 2, Rgt(F) = 0.071, wRref(F2) = 0.176, T = 193 K.
Irrgang T.   +3 more
doaj   +1 more source

Welten erzählen. Narrative Evokation des (Un-)Möglichen

open access: yesDiegesis: Interdisziplinäres E-Journal für Erzählforschung, 2012
Tagungsbericht zu / Conference report of:3. Wuppertaler Graduiertenforum Narratologie, organisiert von Christoph Bartsch (Wuppertal) und Christiane Scheeren (Bayreuth/Wuppertal), AG Erzählforschung der Universität Wuppertal, 14.-16.06 ...
Frauke Bode
doaj  

"Look it up on the Web": Approaches to the Analysis of Clip-Based Knowledge Communication

open access: yesForum: Qualitative Social Research
Knowledge, especially useful knowledge, is increasingly disseminated and acquired through short videos clips circulating on the internet or distributed via social networks.
Bernt Schnettler, Tom Kaden, Lisa Voigt
doaj   +1 more source

Crystal structure of cis-bis[2-(diphenylphosphinoaminato)- 4-methylpyridine]platinum(II), Pt(C18H16N2P)2

open access: yesZeitschrift für Kristallographie - New Crystal Structures, 2006
C36H32N4P2Pt, monoclinic, C12/c1 (no. 15), a = 22.183(1) Å, b = 10.4130(6) Å, c = 15.2670(9) Å, β = 118.038(5)°, V = 3112.7 Å3, Z = 4, Rgt(F) = 0.024, wRref(F2) = 0.069, T = 193 K.
Schmalz T.   +3 more
doaj   +1 more source

Implications of Thermal Weakening and Magma Compressibility for Volcano Monitoring

open access: yesJournal of Geophysical Research: Solid Earth, Volume 131, Issue 9, September 2026.
Abstract Magmatic intrusion and volcanic deformation are traditionally approximated with an inflating cavity in an elastic halfspace. Various analytical models predict surface displacement as a function of pressure or volume change, depth, and elastic crustal properties.
A. Spang   +4 more
wiley   +1 more source

Trace Element Partitioning Between Saline Aqueous Fluids and Subducted Metasediments, and the Origin of the “Sediment Fingerprint” in Arc Magmas

open access: yesGeochemistry, Geophysics, Geosystems
Isotopic and elemental signatures in arc magmas bear similarities to marine sediments from the forearc. Partial melts of subducted sediments were previously invoked as the predominant carrier of material between the slab and mantle wedge, whereas aqueous
M. Putak Juriček   +2 more
doaj   +1 more source

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