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Littérature scientifique sur le sujet « Rif2 »

Auteur : Grafiati

Publié le 9 mars 2023

Mis à jour le 19 juillet 2025

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Articles de revues sur le sujet "Rif2"

Fukunaga, Kenzo, Yukinori Hirano, and Katsunori Sugimoto. "Subtelomere-binding protein Tbf1 and telomere-binding protein Rap1 collaborate to inhibit localization of the Mre11 complex to DNA ends in budding yeast." Molecular Biology of the Cell 23, no. 2 (2012): 347–59. http://dx.doi.org/10.1091/mbc.e11-06-0568.

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Chromosome ends, known as telomeres, have to be distinguished from DNA double-strand breaks that activate DNA damage checkpoints. In budding yeast, the Mre11-Rad50-Xrs2 (MRX) complex associates with DNA ends and promotes checkpoint activation. Rap1 binds to double-stranded telomeric regions and recruits Rif1 and Rif2 to telomeres. Rap1 collaborates with Rif1 and Rif2 and inhibits MRX localization to DNA ends. This Rap1-Rif1-Rif2 function becomes attenuated at shortened telomeres. Here we show that Rap1 acts together with the subtelomere-binding protein Tbf1 and inhibits MRX localization to DNA

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Craven, Rolf J., and Thomas D. Petes. "Dependence of the Regulation of Telomere Length on the Type of Subtelomeric Repeat in the Yeast Saccharomyces cerevisiae." Genetics 152, no. 4 (1999): 1531–41. http://dx.doi.org/10.1093/genetics/152.4.1531.

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Abstract In the yeast Saccharomyces cerevisiae, chromosomes terminate with ∼400 bp of a simple repeat poly(TG1-3). Based on the arrangement of subtelomeric X and Y′ repeats, two types of yeast telomeres exist, those with both X and Y′ (Y′ telomeres) and those with only X (X telomeres). Mutations that result in abnormally short or abnormally long poly(TG1-3) tracts have been previously identified. In this study, we investigated telomere length in strains with two classes of mutations, one that resulted in short poly(TG1-3) tracts (tel1) and one that resulted in elongated tracts (pif1, rap1-17,

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Bonetti, Diego, Carlo Rinaldi, Jacopo Vertemara, et al. "DNA binding modes influence Rap1 activity in the regulation of telomere length and MRX functions at DNA ends." Nucleic Acids Research 48, no. 5 (2019): 2424–41. http://dx.doi.org/10.1093/nar/gkz1203.

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Abstract The cellular response to DNA double-strand breaks (DSBs) is initiated by the Mre11–Rad50–Xrs2 (MRX) complex that has structural and catalytic functions. MRX association at DSBs is counteracted by Rif2, which is known to interact with Rap1 that binds telomeric DNA through two tandem Myb-like domains. Whether and how Rap1 acts at DSBs is unknown. Here we show that Rif2 inhibits MRX association to DSBs in a manner dependent on Rap1, which binds to DSBs and promotes Rif2 association to them. Rap1 in turn can negatively regulate MRX function at DNA ends also independently of Rif2. In fact,

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Hirano, Yukinori, Kenzo Fukunaga, and Katsunori Sugimoto. "Rif1 and Rif2 Inhibit Localization of Tel1 to DNA Ends." Molecular Cell 33, no. 3 (2009): 312–22. http://dx.doi.org/10.1016/j.molcel.2008.12.027.

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Shi, Tianlai, Richard D. Bunker, Stefano Mattarocci, et al. "Rif1 and Rif2 Shape Telomere Function and Architecture through Multivalent Rap1 Interactions." Cell 153, no. 6 (2013): 1340–53. http://dx.doi.org/10.1016/j.cell.2013.05.007.

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Pobiega, Sabrina, Olivier Alibert, and Stéphane Marcand. "A new assay capturing chromosome fusions shows a protection trade-off at telomeres and NHEJ vulnerability to low-density ionizing radiation." Nucleic Acids Research 49, no. 12 (2021): 6817–31. http://dx.doi.org/10.1093/nar/gkab502.

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Abstract Chromosome fusions threaten genome integrity and promote cancer by engaging catastrophic mutational processes, namely chromosome breakage–fusion–bridge cycles and chromothripsis. Chromosome fusions are frequent in cells incurring telomere dysfunctions or those exposed to DNA breakage. Their occurrence and therefore their contribution to genome instability in unchallenged cells is unknown. To address this issue, we constructed a genetic assay able to capture and quantify rare chromosome fusions in budding yeast. This chromosome fusion capture (CFC) assay relies on the controlled inacti

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Li, Bibo, and Titia de Lange. "Rap1 Affects the Length and Heterogeneity of Human Telomeres." Molecular Biology of the Cell 14, no. 12 (2003): 5060–68. http://dx.doi.org/10.1091/mbc.e03-06-0403.

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Telomere length is controlled in part by cis-acting negative regulators that limit telomere extension by telomerase. In budding yeast, the major telomere length regulator scRap1 binds to telomeric DNA and acts to inhibit telomere elongation in cis. Because the human Rap1 ortholog hRap1 does not bind to telomeric DNA directly but is recruited to telomeres by TRF2, we examined its role in telomere length control. The data are consistent with hRap1 being a negative regulator of telomere length, indicating functional conservation. Deletion mapping confirmed that hRap1 is tethered to telomeres thro

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Bradley, Gregory W., John H. Holloway, Han Joong Koh, David G. Morris, and Paul G. Watson. "4-(Difluoroiodo)tricyclene, an isolable compound of type RIF2 from an aliphatic iodide." Journal of the Chemical Society, Perkin Transactions 1, no. 22 (1992): 3001. http://dx.doi.org/10.1039/p19920003001.

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Poschke, Heiko, Martina Dees, Michael Chang, et al. "Rif2 Promotes a Telomere Fold-Back Structure through Rpd3L Recruitment in Budding Yeast." PLoS Genetics 8, no. 9 (2012): e1002960. http://dx.doi.org/10.1371/journal.pgen.1002960.

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Zhang, Ling-Li, Zhenfang Wu, and Jin-Qiu Zhou. "Tel1 and Rif2 oppositely regulate telomere protection at uncapped telomeres in Saccharomyces cerevisiae." Journal of Genetics and Genomics 45, no. 9 (2018): 467–76. http://dx.doi.org/10.1016/j.jgg.2018.09.001.

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Thèses sur le sujet "Rif2"

ANBALAGAN, SAVANI. "Role of saccharomyces cerevisiae Rif1 and Rif2 proteins in protection of telomeres." Doctoral thesis, Università degli Studi di Milano-Bicocca, 2013. http://hdl.handle.net/10281/43717.

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Eukaryotic cells distinguish their chromosome ends from accidental DNA double-strand breaks (DSBs) by packaging them into protective structures called telomeres that prevent DNA repair/recombination activities. In this work, we investigated the role of key telomeric proteins in protecting Saccharomyces cerevisiae telomeres from degradation. We show that the shelterin-like proteins Rif1, Rif2, and Rap1 inhibit nucleolytic processing at both de novo and native telomeres during G1 and G2 cell cycle phases, with Rif2 and Rap1 showing the strongest effects. Also Yku prevents telomere resection in G

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MARTINA, MARINA. "Roles of shelterin-like proteins and yku in saccharomyces cerevisiae telomere homeostasis." Doctoral thesis, Università degli Studi di Milano-Bicocca, 2013. http://hdl.handle.net/10281/41884.

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Telomeres are specialized nucleoprotein complexes that distinguish the natural ends of linear chromosomes from intrachromosomal double-strand breaks. In fact, telomeres are protected from DNA damage checkpoints, homologous recombination or end-to-end fusions that normally promote repair of intrachromosomal DNA breaks. When chromosome end protection fails, dysfunctional telomeres are targeted by the DNA repair and recombination apparatus, whose outcomes range from the generation of chromosomal abnormalities, general hallmarks for human cancer cells, to permanent cell cycle arrest and cell death

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Engels, Silke. "Sugars in early and late polyketide biosynthesis functional studies of rifL, rifK and rifM in rifamycin biosynthesis ; towards the characterisation of a PKS gene cluster from Streptomyces sp. GW2/5831, encoding the biosynthesis of the polycyclic xanthone IB-00208." München Verl. Dr. Hut, 2009. http://d-nb.info/999629123/04.

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Flynn, Luke. "Rift." Digital Commons @ Butler University, 2015. http://digitalcommons.butler.edu/grtheses/268.

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Cornwell, David Graham. "Magma-assisted continental rift margins : the Ethiopian rift." Thesis, University of Leicester, 2007. http://hdl.handle.net/2381/30462.

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Continental rifting and incipient seafloor spreading are observed either side of the main Ethiopian rift (MER). EAGLE (the Ethiopia Afar Geoscientific Lithospheric Experiment) included a 400 km-long profile containing 97 passive seismometers to investigate the change from mechanical to magmatic extension by defining the lithospheric structure and extent of magmatism beneath the rifted northern MER. Changes in crustal structure along the cross-rift profile are imaged using forward modelling, H-kappa stacking and non-linear inversion analyses of receiver functions. The lithospheric structure is

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Arnautov, O. I. "Oculus Rift." Thesis, Sumy State University, 2016. http://essuir.sumdu.edu.ua/handle/123456789/44891.

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Nowadays our world is closely connected with technologies. Changes come in people's lives with technology. People invent new gadgets, tools, machines and more useful things every day. As a rule, all these inventions make our life better and easier.

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Liebrenz, Boris. "Die Rifā‛īya." Universitätsbibliothek Leipzig, 2016. http://nbn-resolving.de/urn:nbn:de:bsz:15-qucosa-202876.

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Dávila, Federico Carlos Eduardo. "Turismo como contribución al desarrollo regional sustentable en Venezuela caso de estudio: Municipio Andrés Bello y Parroquia Jají, Mérida/Venezuela." Rottenburg am Neckar Kersting, 2005. http://www.kersting-verlag.com/riff/titles/riff05/.

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Jackson, Christopher Aiden-Lee. "Structural and stratigraphic evolution of rift basins : the Hammam Faraun area, Suez rift, Egypt." Thesis, University of Manchester, 2002. http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.488323.

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This project aims to integrate structural and stratigraphic data from the Hammam Faraun area, Suez rift, Egypt, to investigate the temporal and spatial evolution of normal fault zones, fault arrays and fault-related folds in extensional settings, and the control the evolving structural style has on syn-rift depositional patterns and sequence stratigraphy. Structural and stratigraphic data from across the Hammam Faraun fault block suggests that during the early stages of rifting deformation was distributed across the fault block on numerous short (1-4 km), low displacement (<1 km) fault segment

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Flotté, Nicolas. "Caractérisation structurale et cinématique d'un rift sur détachement : le rift de Corinthe-Patras, Grèce." Paris 11, 2003. http://www.theses.fr/2003PA112132.

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Une étude structurale de la marge sud du rift de Corinthe montre l'existence d'un détachement quaternaire qui traverse le nord du Péloponnèse du golfe Saronique au golfe de Patras, sur plus de 150km. Sa partie à terre est aujourd'hui inactive, avec un pendage actuel à l'émergence de 30-35ʿN et s'aplatissant vers le nord jusqu'à 0-10ʿN puis augmentant progressivement de pendage sous le golfe. D'autres failles normales, à plus fort pendage nord, affectent le toit du détachement et se sont progressivement branchées dessus. La restauration en profondeur suggère qu'il se prolonge sous le golfe dans

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Livres sur le sujet "Rif2"

Europa, LINCOM, ed. Texts for linguistic analysis: Glossed narratives in Tarifit Berber. Lincom, 2008.

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Cody, Liza. Rift. Collins, 1988.

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Pfahler, Martin. £Riff. Revolver Archiv für aktuelle Kunst, 2003.

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Jean, James. Rift. Chronicle, 2010.

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Cody, Liza. Rift. Collins, 1989.

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Birch, Beverley. Rift. Egmont, 2006.

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Richard, Cox. Rift. Random House Publishing Group, 2004.

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Peter, Cole. Rift. Station Hill Press, 1989.

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Peter, Cole. Rift. Grenfell Press, 1986.

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Cody, Liza. Rift. Arrow Bks., 1994.

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Chapitres de livres sur le sujet "Rif2"

McKittrick, Katherine. "Rift." In Keywords in Radical Geography: Antipode at 50. John Wiley & Sons, Inc., 2019. http://dx.doi.org/10.1002/9781119558071.ch45.

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Smith, Nathan. "Rift Table." In Public Interiority. Routledge, 2024. http://dx.doi.org/10.4324/9781003493501-29.

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Creaven, Sean. "Epidemiological rift." In Contagion Capitalism. Routledge, 2023. http://dx.doi.org/10.4324/9781003437215-5.

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Abusamra, Khawla. "Rift Valley Fever." In Uveitis. Springer International Publishing, 2020. http://dx.doi.org/10.1007/978-3-030-52974-1_36.

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Kahloun, Rim, Imen Ksiaa, and Sonia Zaouali. "Rift Valley Fever." In Emerging Infectious Uveitis. Springer International Publishing, 2017. http://dx.doi.org/10.1007/978-3-319-23416-8_14.

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Scoon, Roger N. "The Gregory Rift." In Geology of National Parks of Central/Southern Kenya and Northern Tanzania. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-73785-0_5.

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Misra, Achyuta Ayan, Neeraj Sinha, and Soumyajit Mukherjee. "The Gop Rift." In Atlas of Structural Geological Interpretation from Seismic Images. John Wiley & Sons, Ltd, 2018. http://dx.doi.org/10.1002/9781119158332.ch44.

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Joordens, Steve, Aakriti Kapoor, and Bob Hofman. "Let's Riff Off RIFS (Relevant, Interesting, Fun, and Social)." In Advances in Early Childhood and K-12 Education. IGI Global, 2019. http://dx.doi.org/10.4018/978-1-5225-8009-6.ch010.

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Online learning allows one to escape traditional constraints and to create learning experiences that allow interactions, and support learning, that would be difficult or impossible in brick and mortar contexts. In this chapter, the authors present a new RIFS taxonomy (Relevance, Interestingness, Fun, and Sociality) to highlight the factors that can make a learning experience especially engaging. They then discuss what they want students to learn when they are engaged in support of 21st century learning. With this context, they describe an initiative called The Global Teenager Project as a concrete example of how, with heavy support from online technologies, these factors can be combined to produce deep learning that students truly find meaningful.

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"RIT2." In Encyclopedia of Signaling Molecules. Springer International Publishing, 2018. http://dx.doi.org/10.1007/978-3-319-67199-4_103331.

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"rift." In Dictionary Geotechnical Engineering/Wörterbuch GeoTechnik. Springer Berlin Heidelberg, 2014. http://dx.doi.org/10.1007/978-3-642-41714-6_182197.

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Actes de conférences sur le sujet "Rif2"

Roy, Protik, and Partha Roy Chaudhuri. "A Numerical Study on the Sensing Characteristics of Raman-Induced Frequency Shift." In JSAP-Optica Joint Symposia. Optica Publishing Group, 2024. https://doi.org/10.1364/jsapo.2024.19p_c43_14.

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We present here an analysis of the sensing properties associated with the Raman-induced frequency shift (RIFS). By employing a conventional step index chalcogenide fiber and utilizing the thermo-optic properties of the material, we investigate the temperature-sensing capabilities facilitated by RIFS.

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Skogdalen, Jon Espen, Stein Haugen, Frode Heldal, et al. "Analysis of Barriers in Marine Operations on Offshore Oil Installations." In ASME 2009 28th International Conference on Ocean, Offshore and Arctic Engineering. ASMEDC, 2009. http://dx.doi.org/10.1115/omae2009-79341.

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The project Risk Modeling – Integration of Organizational, Human and Technical factors is developing a model for quantifying barrier performance related to major risk hazards (OMT-model). The model combines knowledge relating to organizational, human and technical aspects, and is developed in close relationship between research centers, universities and offshore operators. The OMT-model has been tested for process leakages on onshore plants with good results. The same methodology has been used to identify the risk influence factors (RIF) — or Performance Shaping Factors — related to marine ope

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Farid, Farzad, Raed Lubbad, and Kenneth Eik. "A Hybrid Bayesian Belief Network Model for Risk Modeling of Arctic Marine Operations." In ASME 2014 33rd International Conference on Ocean, Offshore and Arctic Engineering. American Society of Mechanical Engineers, 2014. http://dx.doi.org/10.1115/omae2014-23926.

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Optimizing the design of offshore structures to withstand ice loads is a challenging task and various efforts are under way to develop robust concepts with acceptable structural safety. To ameliorate the deficiencies of structural design, as well as to reduce the costs of such Arctic offshore field developments, ice management operations may be considered to reduce the ice severity. Ice management in sea ice will typically involve use of 1 to 4 icebreakers depending on the operating environment. The ice management fleet is aimed at protecting the offshore installation by breaking the incoming

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Wu, Song, and Michael S. Lew. "RIFF." In MM '14: 2014 ACM Multimedia Conference. ACM, 2014. http://dx.doi.org/10.1145/2647868.2654994.

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Yunus, F. A. M. "Palinspastic Reconstruction of X Block, Anggursi Sub-Basin." In Indonesian Petroleum Association - 46th Annual Convention & Exhibition 2022. Indonesian Petroleum Association, 2022. http://dx.doi.org/10.29118/ipa22-sg-135.

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North Anggursi Sub-basin is one of the sub-basins in the North West Java Basin, located on northern of North West Java Basin. North Anggursi Sub-basin regionally was a sinistral pull-apart basin with northeast-southwest orientation which the direction of the extension was east west at Eocene. This subbasin is a back-arc basin during the Eocene to Oligocene. The dynamics of the North Anggursi Sub-basin were analysed using the palinspastic reconstruction method using 2D seismic lines which have east-west direction and biostratigraphy data. This analysis was carried out to determine the tectonic

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Elling, Reece P., Carol A. Stein, Seth Stein, Jonas Kley, G. Randy Keller, and Michael Wysession. "THE MIDCONTINENT RIFT: A RIFT-LIP HYBRID." In GSA Annual Meeting in Seattle, Washington, USA - 2017. Geological Society of America, 2017. http://dx.doi.org/10.1130/abs/2017am-304904.

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Beenfeldt, J. "New Insights Into The Tertiary Petroleum Systems of The East Java Sea and Southern Makassar Strait, Indonesia." In Indonesian Petroleum Association - 46th Annual Convention & Exhibition 2022. Indonesian Petroleum Association, 2022. http://dx.doi.org/10.29118/ipa22-g-94.

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Modern broadband seismic data provides new insight into the Eocene-Miocene syn- to early post-rift sections of the East Java Sea (North Madura) and South Makassar Basin. Previous subsurface imaging suffered from shallow imaging obstacles and “hard” Eocene-Miocene carbonates, which render the interpretation of basement and overlying early syn-rift sections difficult. Thickness and distribution of these syn-sift sections differ significantly when comparing the North Madura area and the South Makassar Basin. Late syn- and early post-rift carbonate development also differs significantly in that a

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Salah, Mohamed, and Ramy Raafat Ahmed. "Velocity Modelling and Depth Conversion Uncertainty Mitigation in GS327 Oil Field, in Gulf of Suez Basin." In GOTECH. SPE, 2025. https://doi.org/10.2118/224602-ms.

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Abstract The Gulf of Suez rift initiated in the Late Oligocene, probably propagating northwards, and intersecting a major east-west structural boundary of Late Eocene age at the latitude of Suez City. North of Suez, extension was more diffuse but mostly focused on the Manzala rift that is presently buried beneath the Nile Delta. Earliest syn-rift, mainly continental sediments (Chattian-Aquitanian) consisted of red beds containing minor basalts. Marine Oligocene strata are presently only proven from the southernmost Gulf, at the juncture with the northern Red Sea. By the Aquitanian, a shallow t

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Tolkunov, A., S. Stovba, E. Dvorianin, and B. Krivchenkov. "Dnieper Donets Rift Basin, Ukraine - Post-rift evolution." In 58th EAEG Meeting. EAGE Publications BV, 1996. http://dx.doi.org/10.3997/2214-4609.201409094.

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Stein, Carol A., Seth Stein, Jonas Kley, et al. "NORTH AMERICA’S MIDCONTINENT RIFT: WHEN RIFT MET LIP." In 50th Annual GSA North-Central Section Meeting. Geological Society of America, 2016. http://dx.doi.org/10.1130/abs/2016nc-275272.

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Rapports d'organisations sur le sujet "Rif2"

Cecile, M. P., B. S. Norford, G. S. Nowlan, and T. T. Uyeno. Lower Paleozoic stratigraphy and geology, Richardson Mountains, Yukon (with stratigraphic and paleontological appendices). Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/329454.

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The Richardson Trough was a rift basin on the southern margin of an ancestral Iapetus Ocean. It was part of a complex paleogeography that included at least two major rift basins on western Franklinian and northern Cordilleran continental shelves. This paleogeography included the Ogilvie Arch, Porcupine Platform, Blackstone 'supra-basin', Babbage Basin, Husky Lakes Arch, Richardson Trough, Mackenzie Arch, Lac des Bois Platform, and the White Mountains and Campbell uplifts. The Richardson Trough was the failed arm of a triple rift system that formed when an early Paleozoic Iapetus Ocean develope

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Keen, C. E., K. Dickie, L. T. Dafoe, et al. Rifting and evolution of the Labrador-Baffin Seaway. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321854.

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The evolution of the 2000 km long Mesozoic rift system underlying the Labrador-Baffin Seaway is described, with emphasis on results from geophysical data sets, which provide the timing, sediment thickness, and crustal structure of the system. The data sets include seismic reflection and refraction, gravity, and magnetic data, with additional constraints provided by near-surface geology and well data. Many features that characterize rift systems globally are displayed, including: wide and narrow rift zones; magma-rich and magma-poor margin segments; exhumation of continental mantle in distal, m

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Kleinrock, Martin C., Peter R. Shaw, and Deborah K. Smith. Seafloor Characterization/Galapagos Propagating Rift. Defense Technical Information Center, 1993. http://dx.doi.org/10.21236/ada272001.

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Sharma, A., P. Thubert, B. Rijsman, and D. Afanasiev. RIFT: Routing in Fat Trees. Edited by T. Przygienda and J. Head. RFC Editor, 2025. https://doi.org/10.17487/rfc9692.

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Gregersen, U., P. C. Knutz, G. K. Pedersen, et al. Stratigraphy of the West Greenland Margin. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321849.

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The stratigraphy and the geological evolution of the West Greenland margin from the Labrador Sea to Baffin Bay in both the onshore and offshore areas are described. The primary data sets include seismic reflection surveys, wells, and outcrops. In addition, seabed samples, seismic refraction and magnetic data, onshore and offshore maps, and stratigraphic compilations were used. The basins of the West Greenland continental margin are described in three regions from the south to the north: southern West Greenland basins, central West Greenland basins, and northern West Greenland basins. Each regi

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Guth, Alexandria. Maps of the Southern Kenya Rift. Geological Society of America, 2014. http://dx.doi.org/10.1130/2014.dmch016.

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Short, Kevin R. The Anzus Rift: The Politics of the Matter. Defense Technical Information Center, 1999. http://dx.doi.org/10.21236/ada388821.

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Ohler, Fritz, and Anton Geyer. Zwischenevaluierung der RIF 2000 Regionale Impulsförderung. Technopolis Forschungs- und Beratungsges.m.b.H, 2005. http://dx.doi.org/10.22163/fteval.2005.184.

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Turner, E. C. Mesoproterozoic Borden Basin, northern Baffin Island. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321825.

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The unmetamorphosed and nearly undeformed late Mesoproterozoic Borden Basin on northern Baffin Island exhibits sag, rift, and foreland-basin-like phases. A thin, partly subaqueous basal basalt is overlain by mature shallow-marine quartz arenite, upward-deepening siltstone and shale (marking the beginning of rifting), a complex suite of rift-delineated carbonate units containing two dramatic internal unconformities, and a flysch-molasse-like succession containing evidence of sediment derivation from the Grenville Orogen. Geochronological data indicate that deposition of most of the succession t

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Dafoe, L. T., K. J. DesRoches, and G. L. Williams. A structural and stratigraphic framework for the western Davis Strait region. Natural Resources Canada/CMSS/Information Management, 2022. http://dx.doi.org/10.4095/321831.

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Western Davis Strait lies within the Labrador-Baffin Seaway rift system, which began forming in the Early Cretaceous as Greenland separated from North America. At chron C27n (Danian), regional seafloor spreading began, as well as significant magmatism. The opening direction changed from southeast-northwest to more north-south in the Thanetian-Ypresian between chrons C25n and C24n, resulting in significant strike-slip motion through the Davis Strait region until seafloor spreading ended at chron C13, near the Eocene-Oligocene boundary. This tectonism has influenced the stratigraphy preserved in

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