Massé, L., Faugères, J.-C., Bernat, M., Pujos, A. & Mézerais, M.-L. A 600,000-year report of Antarctic Bottom Water exercise inferred from sediment textures and buildings in a sediment core from the Southern Brazil Basin. Paleoceanography 9, 1017–1026 (1994).
Hernández-Molina, F. J. et al. Giant mounded drifts within the Argentine Continental Margin: Origins, and world implications for the historical past of thermohaline circulation. Mar. Pet. Geol. 27, 1508–1530 (2010).
Ivanova, E. et al. Late Pliocene–Pleistocene stratigraphy and historical past of formation of the Ioffe calcareous contourite drift, Western South Atlantic. Mar. Geol. 372, 17–30 (2016).
Ivanova, E., Borisov, D., Dmitrenko, O. & Murdmaa, I. Hiatuses within the late Pliocene-Pleistocene stratigraphy of the Ioffe calcareous contourite drift, western South Atlantic. Mar. Pet. Geol. 111, 624–637 (2020).
Ivanova, E. V., Borisov, D. G., Murdmaa, I. O., Ovsepyan, E. A. & Stow, D. Contourite techniques across the northern exit from the Vema Channel. Mar. Geol. 449, 106835 (2022).
Sivkov, V. V., Bashirova, L. D., Dorokhova, E. V., Kapustina, M. V. & Ponomarenko, E. P. Study of the Contourite Drift north of the Kane Gap (japanese equatorial Atlantic). Russ. J. Earth Sci. 19, 1–9 (2019).
Glazkova, T. et al. Sedimentary processes within the Discovery Gap (Central–NE Atlantic): An instance of a deep marine gateway. Deep Sea Res. Part I Oceanogr. Res. Pap. 180, 103681 (2022).
Peive, A. A., Savel’eva, G. N., Skolotnev, S. G. & Simonov, V. A. Structure and Deformations of the Crust-Mantle Boundary Zone within the Vema Fracture Zone, Central Atlantic. Geotectonics 35, 12–29 (2001).
Ligi, M., Cuffaro, M., Muccini, F. & Bonatti, E. Generation and evolution of the oceanic lithosphere within the North Atlantic. La Riv. del Nuovo Cim. 45, 587–659 (2022).
Kastens, Okay. et al. The Vema Transverse Ridge (Central Atlantic). Mar. Geophys. Res. 20, 533–556 (1998).
Rebesco, M., Hernández-Molina, F. J., Van Rooij, D. & Wåhlin, A. Contourites and related sediments managed by deep-water circulation processes: State-of-the-art and future issues. Mar. Geol. 352, 111–154 (2014).
Thran, A. C., Dutkiewicz, A., Spence, P. & Müller, R. D. Controls on the worldwide distribution of contourite drifts: Insights from an eddy-resolving ocean mannequin. Earth Planet. Sci. Lett. 489, 228–240 (2018).
Flanders Marine Institute Renard Centre of Marine Geology Ugent. Global contourite distribution database, model 3 Citable as knowledge publication. (2019). https://doi.org/10.14284/346.
Westall, F., Rossi, S. & Mascle, J. Current-controlled sedimentation within the Equatorial Atlantic: Examples from the southern margin of the Guinea Plateau and the Romanche Fracture Zone. Sediment. Geol. 82, 157–171 (1993).
McCartney, M. S., Bennett, S. L. & Woodgate-Jones, M. E. Eastward movement via the Mid-Atlantic Ridge at 11°N and Its Influence on the Abyss of the Eastern Basin. J. Phys. Oceanogr. 21, 1089–1121 (1991).
Fischer, J., Rhein, M., Schott, F. & Stramma, L. Deep water lots and transports within the Vema Fracture Zone. Deep Sea Res. Part I Oceanogr. Res. Pap. 43, 1067–1074 (1996).
Rhein, M., Stramma, L. & Krahmann, G. The spreading of Antarctic backside water within the tropical Atlantic. Deep Sea Res. Part I Oceanogr. Res. Pap. 45, 507–527 (1998).
Demidov, A. N., Dobrolyubov, S. A., Morozov, E. G. & Tarakanov, R. Y. Transport of backside waters via the Vema Fracture Zone within the Mid-Atlantic ridge. Dokl. Earth Sci. 416, 1120–1124 (2007).
Morozov, E. G., Demidov, A. N., Tarakanov, R. Y. & Zenk, W. Abyssal Channels within the Atlantic Ocean (Springer Netherlands, 2010). https://doi.org/10.1007/978-90-481-9358-5.
Morozov, E. G., Tarakanov, R. Y., Frey, D. I., Demidova, T. A. & Makarenko, N. I. Bottom water flows within the tropical fractures of the Northern Mid-Atlantic Ridge. J. Oceanogr. 74, 147–167 (2018).
Heezen, B. C., Gerard, R. D. & Tharp, M. The Vema fracture zone within the equatorial Atlantic. J. Geophys. Res. 69, 733–739 (1964).
Van Andel, T. H., Von Herzen, R. P. & Phillips, J. D. The Vema fracture zone and the tectonics of transverse shear zones in oceanic crustal plates. Mar. Geophys. Res. 1, 261–283 (1971).
Deville, E. et al. Tectonics and sedimentation interactions within the east Caribbean subduction zone: An overview from the Orinoco delta and the Barbados accretionary prism. Mar. Pet. Geol. 64, 76–103 (2015).
Morozov, E. G., Frey, D. I., Neiman, V. G., Makarenko, N. I. & Tarakanov, R. Y. Extreme transport velocities of Antarctic Bottom Water movement via the deep Vema Channel. Doklady Earth Sciences 486, 659–662 (2019).
Kastens, Okay. A., Macdonald, Okay. C., Miller, S. P. & Fox, P. J. Deep tow research of the Vema Fracture Zone: 2. Evidence for tectonism and backside currents within the sediments of the remodel valley flooring. J. Geophys. Res. Solid Earth 91, 3355–3367 (1986).
Eittreim, S. & Ewing, J. Vema fracture zone remodel fault. Geology 3, 555–558 (1975).
Perch-Nielsen, Okay. et al. Site 353: Vema fracture zone. In Initial Reports of the Deep Sea Drilling Project, 39 (U.S. Government Printing Office, 1977). https://doi.org/10.2973/dsdp.proc.39.102.1977.
Shanmugam, G. 50 years of the turbidite paradigm (Nineteen Fifties–Nineties): Deep-water processes and facies fashions—A important perspective. Mar. Pet. Geol. 17, 285–342 (2000).
Benson, W. E., Gerard, R. D. & Hay, W. W. Summary and conclusions. In Initial Reports of the Deep Sea Drilling Project, 4 (U.S. Government Printing Office, 1970). https://doi.org/10.2973/dsdp.proc.4.127.1970.
Lagabrielle, Y. et al. Vema Fracture Zone (central Atlantic): Tectonic and magmatic evolution of the median ridge and the japanese ridge-Transform intersection area. J. Geophys. Res. 97, 17331 (1992).
Uenzelmann-Neben, G. & Gohl, Okay. The Agulhas Ridge, South Atlantic: The peculiar construction of a fracture zone. Mar. Geophys. Res. 25, 305–319 (2004).
Scrutton, R. A. & Stow, D. A. V. Seismic proof for Early Tertlary bottom-current managed deposition within the Charlie Gibbs Fracture Zone. Mar. Geol. 56, 325–334 (1984).
Hernández-Molina, F. J. et al. Contourites and combined depositional techniques: A paradigm for deepwater sedimentary environments. In Deepwater Sedimentary Systems 301–360 (Elsevier, 2022). https://doi.org/10.1016/B978-0-323-91918-0.00004-9.
Bonatti, E. et al. Mantle thermal pulses beneath the Mid-Atlantic Ridge and temporal variations within the formation of oceanic lithosphere. Nature 423, 499–505 (2003).
Vangriesheim, A. Antarctic Bottom Water movement via the Vema Fracture Zone. Ocean. Acta 3, 199–207 (1980).
GEBCO Compilation Group. GEBCO_2022 Grid. (2022). https://doi.org/10.5285/e0f0bb80-ab44-2739-e053-6c86abc0289c.
Eittreim, S. L., Biscaye, P. E. & Jacobs, S. S. Bottom-water observations within the Vema fracture zone. J. Geophys. Res. 88, 2609 (1983).
Demidov, A. N., Ivanov, A. A., Gippius, F. N. & Dobroliubov, S. A. Transport of deep and backside waters via the mid-Atlantic Ridge within the Vema Fracture Zone. Dokl. Earth Sci. 494, 735–740 (2020).
Morozov, E. G., Tarakanov, R. Y. & Frey, D. I. Bottom Gravity Currents and Overflows in Deep Channels of the Atlantic Ocean (Springer International Publishing, 2021). https://doi.org/10.1007/978-3-030-83074-8.
Bonatti, E. et al. Flexural uplift of a lithospheric slab close to the Vema remodel (Central Atlantic): Timing and mechanisms. Earth Planet. Sci. Lett. 240, 642–655 (2005).
Frey, D. I. et al. Multiple abyssal jets flowing into the Vema deep, Romanche fracture zone. J. Geophys. Res. Ocean. 128, (2023).
Richter, C., Valet, J.-P. & Solheid, P. A. Rock magnetic properties ofsediments from Ceara Rise (Site 929): Implications for the origin of the magnetic susceptibility sign. In Proceedings of the Ocean Drilling Program. Scientific Results 154 (eds. Shackleton, N., Curry, W., Richter, C. & Bralower, T.) 169–179 (1997).
Milliman, J. D., Summerhayes, C. P. & Barretto, H. T. Quaternary sedimentation on the amazon continental margin: A mannequin. Geol. Soc. Am. Bull. 86, 610 (1975).
Damuth, J. E. Late Quaternary sedimentation within the western equatorial Atlantic. Geol. Soc. Am. Bull. 88, 695 (1977).
Maslin, M. & Mikkelsen, N. Amazon Fan mass-transport deposits and underlying interglacial deposits: Age estimates and fan dynamics. In Proceedings of the Ocean Drilling Program, 155 Scientific Results (Ocean Drilling Program, 1997). https://doi.org/10.2973/odp.proc.sr.155.220.1997.
Frey, D. I., Morozov, E. G., Fomin, V. V., Diansky, N. A. & Tarakanov, R. Y. Regional modeling of antarctic backside water flows in the important thing passages of the Atlantic. J. Geophys. Res. Ocean. 124, 8414–8428 (2019).
Faugères, J.-C., Stow, D. A. V., Imbert, P. & Viana, A. Seismic options diagnostic of contourite drifts. Mar. Geol. 162, 1–38 (1999).
Rebesco, M. & Stow, D. Seismic expression of contourites and associated deposits: A preface. Mar. Geophys. Res. 22, 303–308 (2001).
Stow, D. A. V., Faugères, J.-C., Howe, J. A., Pudsey, C. J. & Viana, A. R. Bottom currents, contourites and deep-sea sediment drifts: present state-of-the-art. Geol. Soc. Lond. Mem. 22, 7–20 (2002).
Nielsen, T., Knutz, P. C. & Kuijpers, A. Chapter 16 seismic expression of contourite depositional techniques. In Contourites, vol. 60 (eds. Rebesco, M. & Camerlenghi, A. B. T.-D. S.) 301–321 (Elsevier, 2008).
Smillie, Z., Stow, D. & Esentia, I. Deep-sea contourites drifts, erosional options and bedforms. In Encyclopedia of Ocean Sciences 97–110 (Elsevier, 2019). https://doi.org/10.1016/B978-0-12-409548-9.11590-8.
Frey, D., Borisov, D., Fomin, V., Morozov, E. & Levchenko, O. Modeling of backside currents for estimating their erosional-depositional potential within the Southwest Atlantic. J. Mar. Syst. 230, 103736 (2022).
Stow, D. A. V. et al. Bedform-velocity matrix: The estimation of backside present velocity from bedform observations. Geology 37, 327–330 (2009).
Dianskii, N. A., Bagno, A. V. & Zalesny, V. B. Sigma-model for world ocean circulation and its sensitivity to variations in wind friction stresses. Izv. Akad. Nauk Fiz. Atmos. I OKEANA 38, 537–556 (2002).
Frey, D. I., Fomin, V. V., Diansky, N. A., Morozov, E. G. & Neiman, V. G. New mannequin and area knowledge on estimates of Antarctic Bottom Water movement via the deep Vema Channel. Dokl. Earth Sci. 474, 561–564 (2017).
Frey, D. I., Fomin, V. V, Tarakanov, R. Y., Diansky, N. A. & Makarenko, N. I. Bottom water flows within the Vema channel and over the Santos plateau primarily based on the sector and numerical experiments. In The Ocean in Motion: Circulation, Waves, Polar Oceanography (eds. Velarde, M. G., Tarakanov, R. Y. & Marchenko, A. V) 475–485 (Springer International Publishing, 2018). https://doi.org/10.1007/978-3-319-71934-4_29.
Morozov, E. G. et al. Antarctic backside water within the vema fracture zone summary plain language abstract key factors. J. Geophys. Res.: Oceans 128(8). (2023).
Visbeck, M. Deep velocity profiling utilizing lowered acoustic Doppler present profilers: Bottom monitor and inverse options*. J. Atmos. Ocean. Technol. 19, 794–807 (2002).
Egbert, G. D. & Erofeeva, S. Y. Efficient inverse modeling of Barotropic ocean tides. J. Atmos. Ocean. Technol. 19, 183–204 (2002).
Ivanova, E. V. et al. Investigations of lateral sedimentation and water mass properties within the tropical atlantic throughout cruise 60 of the R/V Akademik Ioffe. Oceanology 62, 581–583 (2022).
