149 research outputs found
Transforming work environments: Unveiling the dynamics and impacts of coworking spaces Working beyond boundaries: Redefining work modes and spaces across geographies dossier editorial
Who talks about collaborative spaces, how, and why
Communities in urban contexts and firms in corporate offices have recently started to implement collaborative spaces. Several authors from different disciplines are currently advancing knowledge in this realm. Systematizing this diverse knowledge base helps to advance our understanding of this novel phenomenon. To this end, the present work reviews 29 papers focusing on collaborative spaces. We analyse these papers in terms of contents, research methods, fields of study, authorsâ background, and impact on the academic community. Grounding on this analysis, we outline new relevant research questions and opportunities for future investigations
Is Digitalization Worth the Hassle? Two cases of Innovation Building Operation and Maintenance
Evolution of the Southwest Australian Rifted Continental Margin During Breakup of East Gondwana: Results from IODP Expedition 369
International Ocean Discovery Program Expedition 369 drilled four sites on the southwestern Australian continental margin, in the deep water Mentelle Basin (MB) and on the neighboring Naturaliste Plateau (NP). The drillsites are located on continental crust that continued rifting after seafloor spreading began further north on the Perth Abyssal Plain (PAP) between magnetochrons M11r and M11n (133â132 Ma), ending when spreading began west of the NP between chrons M5n and M3n (126â124 Ma). Drilling recovered the first inâsitu samples of basalt flows overlying the breakup unconformity on the NP, establishing a magnetostratigraphically constrained eruption age of >131â133 Ma and confirming a minimal late Valanginian age for the breakup unconformity (coeval with the onset of PAP seafloor spreading). Petrogenetic modeling indicates the basalts were generated by 25% melting at 1.5 GPa and a potential temperature of 1380â1410 °C, consistent with proximity of the Kerguelen plume during breakup. Benthic foraminiferal fossils indicate that the NP remained at upper bathyal or shallower depths during the last 6 Myr of rifting and for 3â5 Myr after breakup between India and Australia. The limited subsidence is attributed to heat from the nearby Kerguelen plume and PAP spreading ridge. The margin subsided to middle bathyal depths by Albian time and to lower bathyal (NP) or greater (MB) depths by late Paleogene time. Periods of rapid sedimentation accompanied a westward jump of the PAP spreading ridge (108 Ma), rifting on the southern margin (100â84 Ma), and opening of the southern seaway between Australia and Antarctica (60â47 Ma)
Molecular phylogeny of the genus Saguinus (Platyrrhini, Primates) based on the ND1 mitochondrial gene and implications for conservation
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