Published January 31, 2019
| Version v1
Figure
Open
Fig. 13 in Quaternary time scales for the Pontocaspian domain: Interbasinal connectivity and faunal evolution
Creators
- Krijgsman, W.1
- Tesakov, A.2
- Yanina, T.3
- Lazarev, S.1
- Danukalova, G.4
- Van Baak, C.G.C.5
- Agustí, J.6
- Alçiçek, M.C.7
- Aliyeva, E.8
- Bista, D.9
- Bruch, A.10
- Büyükmeriç, Y.11
- Bukhsianidze, M.12
- Flecker, R.9
- Frolov, P.2
- Hoyle, T.M.1
- Jorissen, E.L.1
- Kirscher, U.13
- Koriche, S.A.14
- Kroonenberg, S.B.15
- Lordkipanidze, D.12
- Oms, O.16
- Rausch, L.17
- Singarayer, J.14
- Stoica, M.17
- van de Velde, S.18
- Titov, V.V.19
- Wesselingh, F.P.18
- 1. Department of Earth Sciences, Utrecht University, Budapestlaan 17, Utrecht 3584, The Netherlands
- 2. Geological Institute of the Russian Academy of Sciences, Pyzhevsky 7, Moscow 119017, Russia
- 3. Lomonosov Moscow State University, Moscow 119991, Russia
- 4. Russian Academy of Sciences, Institute of Geology of the Ufimian Scientific Centre, K. Marx St. 16/2, Ufa 450077, Russia
- 5. CASP, West Building, Madingley Rise, Madingley Road, Cambridge CB3 0UD, UK
- 6. ICREA. Institut Català de Paleoecologia Humana i Evolució Social (IPHES), Universitat Rovira i Virgili, Tarragona, Spain
- 7. Department of Geology, Pamukkale University, Denizli 20070, Turkey
- 8. Geological Institute of Azerbaijan (GIA), H. Javid Av. 29A, AZ1143, Baku, Azerbaijan
- 9. BRIDGE, School of Geographical Sciences and Cabot Institute, University of Bristol, University Road, Bristol BS8 1SS, UK
- 10. Senckenberg Forschungsinstitut Senckenberganlage, Frankfurt 25 60325, Germany
- 11. Department of Geological Engineering, Bülent Ecevit University, Incivez/Zonguldak 67100, Turkey
- 12. The National Museum of Georgia, 3 Purtseladze St., 0107, Tbilisi, Georgia
- 13. Earth Dynamics Research Group, Department of Applied Geology, WASM, Curtin University, Perth, Australia
- 14. Department of Meteorology and Centre for Past Climate Change, University of Reading, UK
- 15. Department of Applied Earth Sciences, Delft University of Technology, Delft 2600, The Netherlands
- 16. Fac. de Ciències Universitat Autònoma de Barcelona, E-08193 Bellaterra, Barcelona, Spain
- 17. Department of Paleontology, Bucharest University, Bălcescu Bd. 1, Bucharest 010041, Romania
- 18. Naturalis Biodiversity Center, P.O. Box 9517, Leiden 2300, The Netherlands
- 19. Russian Academy of Sciences, Institute of Arid Zones, Chekhova 41, Rostov-on-Don 344006, Russia
Description
Fig. 13. Map showing potential Akchagylian transgression mechanisms and possible connection points with brief outline of the requirements for each and the observed phenomena each would be able to explain. The main mechanisms discussed are climate driven base level rise and connection with an adjacent basin. Three potential adjacent water bodies are considered as the source of incoming water (Arctic Ocean, Indian Ocean and the Black Sea). For each of the three two potential gateways are suggested.
Notes
Published as part of Krijgsman, W., Tesakov, A., Yanina, T., Lazarev, S., Danukalova, G., Van Baak, C.G.C., Agustí, J., Alçiçek, M.C., Aliyeva, E., Bista, D., Bruch, A., Büyükmeriç, Y., Bukhsianidze, M., Flecker, R., Frolov, P., Hoyle, T.M., Jorissen, E.L., Kirscher, U., Koriche, S.A., Kroonenberg, S.B., Lordkipanidze, D., Oms, O., Rausch, L., Singarayer, J., Stoica, M., van de Velde, S., Titov, V.V. & Wesselingh, F.P., 2019, Quaternary time scales for the Pontocaspian domain: Interbasinal connectivity and faunal evolution, pp. 1-40 in Earth-Science Reviews 188 on page 26, DOI: 10.1016/j.earscirev.2018.10.013, http://zenodo.org/record/5027207
Files
figure.png
Files
(4.6 MB)
| Name | Size | Download all |
|---|---|---|
|
md5:23596dd89520f40ac1c6a07924933816
|
4.6 MB | Preview Download |
Linked records
Additional details
Related works
- Is part of
- Journal article: 10.1016/j.earscirev.2018.10.013 (DOI)
- Journal article: urn:lsid:plazi.org:pub:BB12FFC5FFD5FFE7955D8C3DFF9FFFDF (LSID)
- Journal article: https://zenodo.org/record/5027207 (URL)