Institution
Ensenada Center for Scientific Research and Higher Education
Facility•Ensenada, Mexico•
About: Ensenada Center for Scientific Research and Higher Education is a facility organization based out in Ensenada, Mexico. It is known for research contribution in the topics: Population & Nonlinear system. The organization has 1934 authors who have published 3733 publications receiving 63115 citations.
Papers published on a yearly basis
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TL;DR: Differences in pigmentation, light absorption, and changes in the chlorophyll a fluorescence signal between apical and basal thalli of E. isiforme and Gracilaria damaecornis confirm that Rhodophyta is a highly diverse algal group with respect to antenna composition and photoprotective mechanisms.
Abstract: The success of Rhodophyta in coastal areas is largely determined by their capacity to withstand high-light conditions. To understand the photo-acclimatory response of Rhodophyta, we compared differences in pigmentation, light absorption, and changes in the chlorophyll a fluorescence signal between apical and basal thalli of Eucheuma isiforme, a lutein-predominant species, and Gracilaria damaecornis, a zeaxanthin-predominant species. Variation in the fluorescence signal was characterized after exposure of basal and apical segments of each species to five saturating light levels, and monitoring of the subsequent recovery in the absence and presence of chloramphenicol, an inhibitor of the photosystem II (PSII) repair mechanism. Our results confirm that Rhodophyta is a highly diverse algal group with respect to antenna composition and photoprotective mechanisms. The permanent activation of an energy quencher in the zeaxanthin-predominant species requires switching to antheraxanthin in the low-light response and higher dependence on PSII repair. No such quencher was detected in the lutein-predominant species, which showed no change in relative carotenoid composition, slight differences between apical and basal thalli in PSII pressure, and less dependence on PSII repair. It remains unclear if the combined presence of lutein–zeaxanthin allows effective photoprotection or if other mechanisms (i.e., phycobilisome quenching) may explain the effective photoprotective response shown by E. isiforme. The differences highlighted in this comparison may contribute to explain the distribution and abundance of Rhodophyta in marine coastal areas through understanding differences within the group in their ability to protect the photosynthetic apparatus from absorbing light in excess, and in the metabolic costs of PSII repair.
22 citations
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TL;DR: In this article, the authors study local and regional body-wave arrival times from several seis- mic networks to better define the active regional fault pattern in the epicentral region of the 3 May 1887 Mw 7.5 Sonora, Mexico (southern Basin and Range Province) earthquake.
Abstract: We study local and regional body-wave arrival times from several seis- mic networks to better define the active regional fault pattern in the epicentral region of the 3 May 1887 Mw 7.5 Sonora, Mexico (southern Basin and Range Province) earthquake. We determine hypocenter coordinates of earthquakes that originated between 2003 and 2007 from arrival times recorded by the local network RESNES (Red Sismica del Noreste de Sonora) and stations of the Network of Autonomously Recording Seismographs (NARS)-Baja array. For events between April and December 2007, we also incorporated arrival times from USArray stations located within 150 km of the United States-Mexico border. We first obtained preliminary earthquake loca- tions with the Hypoinverse program (Klein, 2002) and then relocated these initial hypocenter coordinates with the source-specific station term (SSST) method (Lin and Shearer, 2005). Most relocated epicenters cluster in the upper crust near the faults that ruptured during the 1887 earthquake and can be interpreted to be part of its long- lasting series of aftershocks. The region of aftershock activity extends, along the same fault zone, 40-50 km south of the documented southern tip of the 1887 rupture and includes faults in the epicentral region of the 17 May 1913 (Imax VIII, MI 5.0-0.4) and 18 December 1923 (Imax IX, MI 5.7-0.4) Granados-Huasabas, Sonora, earthquakes, which themselves are likely to be aftershocks of the 1887 event. The long aftershock duration can be explained by the unusually large magnitude of the mainshock and by the low slip rates and long mainshock recurrence times of the faults that ruptured in 1887.
22 citations
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Central Maine Community College1, Ensenada Center for Scientific Research and Higher Education2, University of Copenhagen3, Danish Meteorological Institute4, The Cyprus Institute5, International Centre for Theoretical Physics6, Commonwealth Scientific and Industrial Research Organisation7, Swedish Meteorological and Hydrological Institute8, Université du Québec à Montréal9, University of Cape Town10, Boğaziçi University11, Chinese Academy of Sciences12, Sao Paulo State University13, Işık University14, Karlsruhe Institute of Technology15, University of São Paulo16, Facultad de Ciencias Exactas y Naturales17, University of Buenos Aires18, National University of Malaysia19, University of Queensland20, Centre national de la recherche scientifique21, University of New South Wales22, Cooperative Institute for Research in Environmental Sciences23
Abstract: Global warming is likely to cause a progressive drought increase in some regions, but how population and natural resources will be affected is still underexplored. This study focuses on global population and land-use (forests, croplands, pastures) exposure to meteorological drought hazard in the 21st century, expressed as frequency and severity of drought events. As input, we use a large ensemble of climate simulations from the Coordinated Regional Climate Downscaling Experiment, population projections from the NASA-SEDAC dataset, and land-use projections from the Land-Use Harmonization 2 project for 1981–2100. The exposure to drought hazard is presented for five SSPs (SSP1-SSP5) at four Global Warming Levels (GWLs, from 1.5 to 4°C). Results show that considering only Standardized Precipitation Index (SPI; based on precipitation), the combination SSP3-GWL4 projects the largest fraction of the global population (14%) to experience an increase in drought frequency and severity (vs. 1981–2010), with this value increasing to 60% if temperature is considered (indirectly included in the Standardized Precipitation-Evapotranspiration Index, SPEI). With SPEI, considering the highest GWL for each SSP, 8 (for SSP2, SSP4, and SSP5) and 11 (SSP3) billion people, that is, more than 90%, will be affected by at least one unprecedented drought. For SSP5 (fossil-fuelled development) at GWL 4°C, approximately 2·106 km2 of forests and croplands (respectively, 6 and 11%) and 1.5·106 km2 of pastures (19%) will be exposed to increased drought frequency and severity according to SPI, but for SPEI, this extent will rise to 17·106 km2 of forests (49%), 6·106 km2 of pastures (78%), and 12·106 km2 of croplands (67%), with mid-latitudes being the most affected areas. The projected likely increase of drought frequency and severity significantly increases population and land-use exposure to drought, even at low GWLs, thus extensive mitigation and adaptation efforts are needed to avoid the most severe impacts of climate change.we
22 citations
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TL;DR: Data specify an antagonistic relationship between the SIN and MOR during septum formation in the filamentous ascomycete model Neurospora crassa that is, at least in part, coordinated through the GC kinase MST-1.
Abstract: Nuclear DBF2p-related (NDR) kinases constitute a functionally conserved protein family of eukaryotic regulators that control cell division and polarity. In fungi, they function as effector kinases of the morphogenesis (MOR) and septation initiation (SIN) networks and are activated by pathway-specific germinal centre (GC) kinases. We characterized a third GC kinase, MST-1, that connects both kinase cascades. Genetic and biochemical interactions with SIN components and life cell imaging identify MST-1 as SIN-associated kinase that functions in parallel with the GC kinase SID-1 to activate the SIN-effector kinase DBF-2. SID-1 and MST-1 are both regulated by the upstream SIN kinase CDC-7, yet in an opposite manner. Aberrant cortical actomyosin rings are formed in Δmst-1, which resulted in mis-positioned septa and irregular spirals, indicating that MST-1-dependent regulation of the SIN is required for proper formation and constriction of the septal actomyosin ring. However, MST-1 also interacts with several components of the MOR network and modulates MOR activity at multiple levels. MST-1 functions as promiscuous enzyme and also activates the MOR effector kinase COT-1 through hydrophobic motif phosphorylation. In addition, MST-1 physically interacts with the MOR kinase POD-6, and dimerization of both proteins inactivates the GC kinase hetero-complex. These data specify an antagonistic relationship between the SIN and MOR during septum formation in the filamentous ascomycete model Neurospora crassa that is, at least in part, coordinated through the GC kinase MST-1. The similarity of the SIN and MOR pathways to the animal Hippo and Ndr pathways, respectively, suggests that intensive cross-communication between distinct NDR kinase modules may also be relevant for the homologous NDR kinases of higher eukaryotes.
22 citations
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TL;DR: No significant differences were found in the temperature of the onset of behavioural response spasms and equilibrium loss in Ictalurus punctatus maintained in constant and fluctuating temperatures.
22 citations
Authors
Showing all 1956 results
Name | H-index | Papers | Citations |
---|---|---|---|
Scott L. Stephens | 65 | 228 | 14311 |
Stephen V. Smith | 51 | 106 | 9235 |
Rodrigo Vargas | 49 | 183 | 10924 |
Salomon Bartnicki-Garcia | 46 | 96 | 7928 |
Sarah K. Spurgeon | 46 | 358 | 12231 |
Gloria Mark | 46 | 197 | 7426 |
Frank L. Vernon | 45 | 192 | 8765 |
Edwin L. Piner | 42 | 162 | 5020 |
Rafael Kelly | 38 | 142 | 5083 |
Gary J. Axen | 37 | 101 | 5397 |
Yury Orlov | 36 | 191 | 4160 |
Antonio Manuel Lazaro | 35 | 318 | 5219 |
Ingo Horn | 34 | 86 | 5359 |
Miguel F. Lavín | 34 | 86 | 3320 |
Francisco J. Beron-Vera | 32 | 116 | 3282 |