Building Connections in Co-Production Environments

With the impact of the Covid-19 pandemic felt around the globe, consumers look forward to once again being able to engage in communal experiences where relationships with other customers and with service providers are integral parts of ongoing service experiences. The purpose of this study is to provide a framework for service establishments to better understand the communal approach to becoming a service co-creator, helping service providers create more meaningful relationships between their customers when customers are engaging in the service experience in a group and as an individual. We distinguish individual versus group influences that emerge as a result of this unique but growing class of service offerings. We extend knowledge in this area by uncovering the nontangible elements of a co-production experience found to deepen the customer-service provider relationship, which ultimately impacts repeat patronage. We examined these influences in two different co-production environments and subsequently laid the foundation for the need for further research in this area, with the goal of identifying common practices that can enhance co-creation across varied industries

Modeling lymphangiogenesis in a three-dimensional culture system

peer reviewedUnraveling the molecular mechanisms of lymphangiogenesis is hampered by the lack of appropriate in vitro models of three-dimensional (3D) lymph vessel growth which can be used to exploit the potential of available transgenic mice. We developed a potent reproducible and quantifiable 3D-culture system of lymphatic endothelial cells, the lymphatic ring assay, bridging the gap between 2D-in vitro and in vivo models of lymphangiogenesis. Mice thoracic duct fragments are embedded in a collagen gel leading to the formation of lymphatic capillaries containing a lumen as assessed by electron microscopy and immunostaining. This assay phenocopies the different steps of lymphangiogenesis, including the spreading from a preexisting vessel, cell proliferation, migration and differentiation into capillaries. Our study provides evidence for the implication of an individual matrix metalloproteinase, MMP-2, during lymphangiogenesis. The lymphatic ring assay is a robust, quantifiable and reproducible system which offers new opportunities for rapid identification of unknown regulators of lymphangiogenesis

Anaerobic Methane Oxidizers

The anaerobic oxidation of methane (AOM) with sulfate as the final electron acceptor according to (CH4 + SO4 2− → HCO3 − + HS− + H2O) is the major sink of methane in the oceans and hence a significant process in the global carbon cycle and methane budget. Anaerobic methane oxidizing archaea (ANME) and sulfate-reducing bacteria (SRB) are assumed to act as a syntrophic consortium where the archaeal partner activates and metabolizes methane, leading to an intermediate that is scavenged as electron donor by the sulfate-reducing partner. All known anaerobic methanotrophs are related to the methanogenic Euryarchaeota. Recently, much has been learned about the distribution, activity, and physiology of the ANME, however, not a single member of these groups has been obtained in culture and the biochemical functioning of AOM remains unknown

Anaerobic Methane Oxidizers

The anaerobic oxidation of methane (AOM) with sulfate as the final electron acceptor according to the net reaction CH4 + SO42- -> HCO3- -> HS- + H2O is the major sink of methane in the ocean floor and hence a significant process in the marine methane budget and the global carbon cycle. Since its discovery, much has been learned about the distribution of the AOM process, its activity in different settings, and connections to other metabolic reactions in the seafloor. AOM is performed by consortia of anaerobic methane-oxidizing archaea (ANME) and sulfate-reducing bacteria (SRB). Since all known ANME and most of their partner bacteria have so far resisted isolation, the physiology of both organisms has been largely inferred from culture-independent approaches on natural enrichments or enrichment cultures. All known ANME are related to methanogenic Euryarchaeota, and as such they reverse the methanogenesis pathway to activate and completely oxidize methane. The reducing equivalents are shuttled to the partner bacteria, which use them for sulfate reduction. Recently, evidence has been found for ANME that can use nitrate or iron as electron acceptors. The exact mechanisms for the required exchange of reducing equivalents in AOM and their genetic codes are yet poorly understood, but recently discovered accumulations of cytochromes and nanowire connections in the intercellular space of the consortia suggest direct electron transfer between both partners