Published October 31, 2019
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Fig. 7 in Magneto-biostratigraphic age constraints on the palaeoenvironmental evolution of the South Caspian basin during the Early-Middle Pleistocene (Kura basin, Azerbaijan)
Creators
- 1. Paleomagnetic Laboratory «Fort Hoofddijk», Department of Earth Sciences, Utrecht University, Budapestlaan 17, 3584CD, Utrecht, the Netherlands
- 2. Naturalis Biodiversity Center, P.O. Box 9517, 2300RA, Leiden, the Netherlands
- 3. Department of Geology, Faculty of Geology and Geophysics, Bucharest University, Bǎlcescu Bd. 1, 010041, Bucharest, Romania
- 4. CASP, West Building, Madingley Rise, Madingley Road, CB3 0UD, Cambridge, United Kingdom
- 5. M.V. Lomonosov Moscow State University, Geographical Faculty, Leninskiye Gory, 119992, Moscow, Russia
- 6. Institute of Geology ANAS, H. Javid av., 29A, 1143, Baku, Azerbaijan
Description
Fig. 7. Magnetostratigraphy of the Goychay section. In columns, from left to right: Regional (local) stages; Depositional units; Lithological log; Biostratigraphic sampling points: green - mollusc samples, blue - microfauna samples; Magnetic susceptibility (plotted on a logarithmic scale; black line - values for each sample, red line - averaged 3); Inclination; Declination; Interpreted polarity (black - normal, white - reversed). The Akchagylian - Apsheronian transition is drawn based on microfauna (lower limit) and macrofauna (upper limit). (For interpretation of the references to colour in this figure legend, the reader is referred to the Web version of this article.)
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Related works
- Is part of
- Journal article: 10.1016/j.quascirev.2019.105895 (DOI)
- Journal article: urn:lsid:plazi.org:pub:0C22FF88FFDACA728C204932CD7AFF8D (LSID)
- Journal article: https://zenodo.org/record/5020945 (URL)