@article{22c517e48d7342c19184fe6eae9bc06f,
title = "Arctic Ocean Mega Project: Paper 3 - Mesozoic to Cenozoic geological evolution",
abstract = "We present an atlas of paleogeographic and paleotectonic maps which documents major events in the Arctic for 0–157 Ma. We demonstrate that the Mendeleev Ridge has a continental basement. The following chronology of events in the history of the Arctic Ocean is proposed: (1) Jurassic: continental rifting in the area of the Sverdrup-Banks basins and in the area of the present-day Canada Basin; a system of continental-margin volcanic belts formed in the region of Chukotka and the Verkhoyansk-Omolon; (2) Berriasian-Barremian: formation of the continental-margin Verkhoyansk-Chukotka Orogen; fast opening of Canada Basin (~133–125 Ma); (3) Aptian-Albian: formation of continental igneous provinces, rifting and magmatism in the area of the Alpha-Mendeleev ridges; rifting in the Ust{\textquoteright}-Lena, Anisin, North-Chukchi, Podvodnikov and Toll basins; (4) Cenomanian-Campanian: intraplate magmatism in the area of the Alpha-Mendeleev ridges; (5) Campanian-Maastrichtian: a likely start of compressional deformations in the area of the Chukchi Sea; (6) Paleocene: formation of the continental-margin orogen; continental rifting along the present-day Eurasia Basin and the Ust{\textquoteright}-Lena Basin; (7) Early-Middle Eocene: onset of opening of the Eurasia Basin started; (8) Middle-Late Eocene: a major restructuring of paleogeography of the Arctic took place at ca. 45 Ma with subaerial emergence of the Barents and Kara Sea shelves and onset of ultra-slow spreading of the Gakkel Ridge, and start of the epoch of formation of normal and strike-slip faults on the Lomonosov and Alpha-Mendeleev ridges and on the shelves of the Chukchi and East Siberian seas. Paleoclimate is discussed in connection with changes in the paleogeography.",
keywords = "Arctic, Lomonosov Ridge, Amundsen Basin, Nansen Basin, Podvodnikov Basin, North Chukchi Basin, Mendeleev Ridge, Laptev Sea Basin, East Siberian Sea Basin, Gakkel Ridge, Climate change",
author = "Nikishin, {Anatoly M.} and Petrov, {Eugene I.} and Sierd Cloetingh and Freiman, {Sergey I.} and Malyshev, {Nikolay A.} and Morozov, {Andrey F.} and Posamentier, {Henry W.} and Verzhbitsky, {Vladimir E.} and Zhukov, {Nikolay N.} and Ksenia Startseva",
note = "Funding Information: The authors are thankful to Ministry of Natural Resources and Ecology of Russia for the possibility to publish this paper. Discussions with C. Gaina, E. Miller, V. Pease, W. Jokat, J.I. Faleide, S. Drachev, R. Stephenson, D. Franke, A. Escalona, I. Norton, N. Lebedeva-Ivanova, E. Lundin, A. Dor?, E. Weigelt stimulated our work. We are grateful to many Russian geologists from different scientific organizations with which we conducted numerous discussions: L.I. Lobkobsky, V.A. Vernikovsky, S.D. Sokolov, A.K. Khudoley, A.V. Prokopiev, O.V. Petrov, E.V. Shipilov, A.V. Stoupakova, E.A. Gusev, V.A. Poselov, S.N. Kashubin, G.N. Aleksandrova, A.S. Alekseev, V.B. Ershova, A.B. Herman, and others. In the course of studying the Arctic, we had the possibility to conduct scientific discussions with geologists from different companies: Rosneft, ExxonMobil, Statoil, Total, BP, Gazprom Neft, Gazprom. We thank our colleagues E.A. Bulgakova, M.S. Doronina, L.N. Kleschina, V.A. Nikishin, A.B. Popova, M.V. Skaryatin, M.A. Baklan and M.A. Rogov for important contribution in preparation our paleogeographic maps. The work of AMN, SIF, KFS and NNZ was supported by RFBR grants (18-05-70011 and 18-05-00495). We thank Fran?ois Roure, David Mosher and an anonymous reviewer for generous, detailed, and constructive criticism. Funding Information: The authors are thankful to Ministry of Natural Resources and Ecology of Russia for the possibility to publish this paper. Discussions with C. Gaina, E. Miller, V. Pease, W. Jokat, J.I. Faleide, S. Drachev, R. Stephenson, D. Franke, A. Escalona, I. Norton, N. Lebedeva-Ivanova, E. Lundin, A. Dor{\'e}, E. Weigelt stimulated our work. We are grateful to many Russian geologists from different scientific organizations with which we conducted numerous discussions: L.I. Lobkobsky, V.A. Vernikovsky, S.D. Sokolov, A.K. Khudoley, A.V. Prokopiev, O.V. Petrov, E.V. Shipilov, A.V. Stoupakova, E.A. Gusev, V.A. Poselov, S.N. Kashubin, G.N. Aleksandrova, A.S. Alekseev, V.B. Ershova, A.B. Herman, and others. In the course of studying the Arctic, we had the possibility to conduct scientific discussions with geologists from different companies: Rosneft, ExxonMobil, Statoil, Total, BP, Gazprom Neft, Gazprom. We thank our colleagues E.A. Bulgakova, M.S. Doronina, L.N. Kleschina, V.A. Nikishin, A.B. Popova, M.V. Skaryatin, M.A. Baklan and M.A. Rogov for important contribution in preparation our paleogeographic maps. The work of AMN, SIF, KFS and NNZ was supported by RFBR grants ( 18-05-70011 and 18-05-00495 ). We thank Fran{\c c}ois Roure, David Mosher and an anonymous reviewer for generous, detailed, and constructive criticism. Publisher Copyright: {\textcopyright} 2019 Elsevier B.V.",
year = "2021",
month = jun,
doi = "10.1016/j.earscirev.2019.103034",
language = "English",
volume = "217",
journal = "Earth-Science Reviews",
issn = "0012-8252",
publisher = "Elsevier",
}