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(a, a’) optix>GFP primordium stained for GFP, the photoreceptor marker Elav and Cas3*. The expression of the optix-GAL4 driver, as detected by GFP-expression is outlined (in a’). The Cas3* signal is low (a’). (b, b’) optix>+ primordium stained for the G2-marker Cyclin B (CycB) and Dcp-1. Dcp-1 signal is detected in a band of cells anterior to the differentiating wavefront (this latter lacks CycB expression)., Peer reviewed

Additional file 1: Figure S1. A minimal increase in Cdc20Slp1 levels causes sensitivity to MBC and defective mitotic arrest. A. Slp1 protein level was determined from asynchronously growing cells of the indicated genotypes. Cdc2 was used as a loading control. B. Spot growth assay of the indicated strains and condition. C-E. Representative examples of mitotic arrest assay of the indicated strains. Cell cultures were grown at permissive temperature (32ºC) and then shifted to restrictive temperature (18ºC). Samples were taken every hour and the septation index calculated form more than 200 cells in each time point and condition. Representative examples of two independent experiments are shown., Ministerio de Economía y Competitividad Ministerio de Ciencia e Innovación Consejería de Economía, Conocimiento, Empresas y Universidad, Junta de Andalucía Fundación Séneca de la Región de Murcia National Institutes of Health, Peer reviewed

The dataset contains 3 files.-- Information on the methodology and quality control can be found in the files description and references included in the README_NWIberian_DO_1969_2018_V02.txt file, The dataset NWIberian_DO_1969_2018_V02 contains: averaged yearly data from compiled datasets of dissolved oxygen concentration, temperature and salinity at the 27.1 isopycnal level from different cruises between 1969 and 2018, and covering the area 40°- 43°N and 9°-11°W; time series of the potential drivers of the dissolved oxygen change in the region of ENACW formation (45°- 49°N and 9°-20°W) and off the NW Iberian coast (40°- 43°N and 9°-11°W); distributions of sea surface temperature over the area 39°- 55°N and 6°-30°W and averaged over differente time periods; and table with examples from other upwelling regions in terms of concentration and trends of dissolved oxygen, Funding for this dataset was provided by the Spanish Ministry of Science and Innovation through a Personal Técnico de Apoyo grant (PTA2019-017492-I) and the CAPTA project (CAPTA 0062_CAPTA_1_E, POCTEP 2021-2027), ENACWsptseries19692018V02.csv.-- SST_NAtlantic.csv.-- Oxygen_upwelling_systems.csv.-- README_NWIberian_DO_1969_2018_V02.txt, No

Results of the beta regression, assessing the effect of NewAlters on the Abstract Similarity Score., Peer reviewed

Descriptive statistics for the main variables employed in the beta regression analysis., Peer reviewed

Descriptive statistics for variables Abstract Similarity Score and SharedDyad., Peer reviewed

A boxplot, comparing instances of repeated collaborations (SharedDyad = 1) to the rest of project pairs (SharedDyad = 0)., Peer reviewed

An illustrative example of the SharedDyad variable., Peer reviewed

A graphical representation of the 2-step methodological approach., Peer reviewed

A histogram of project-abstract length, measured in word count., Peer reviewed