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| Format: | Dataset Open Access |
| Language: | en |
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PANGAEA
2025
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| Online Access: | https://doi.org/10.1594/PANGAEA.987089 |
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| _version_ | 1867171901926801408 |
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| author | Cannings, Torin Robertson, Alastair H F Kroon, Dick |
| author_facet | Cannings, Torin Robertson, Alastair H F Kroon, Dick |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | We present a c. 12 Ma record of oxygen and carbon stable isotopes from the Island of Cyprus to help constrain the nature and extent of Miocene palaeoceanographic changes in the eastern Mediterranean region. Cyprus includes Neogene deep-sea pelagic sedimentary rocks, which are suitable for stable isotope studies. Our composite geochemical record integrates data from the Lower-Upper Miocene succession at Kottaphi Hill along the northern margin of the Troodos ophiolite, and the Upper Miocene succession at Lapatza Hill to the south of the Kyrenia Range. Calcareous nannofossil biostratigraphy reveals that the composite record spans the Miocene Climatic Optimum's onset to the beginning of the Messinian Salinity Crisis. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_987089 |
| institution | PANGAEA |
| language | en |
| publishDate | 2025 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | δ18O and δ13C stable isotope data from a new composite sediment record, Cyprus (Eastern Mediterranean) Cannings, Torin Robertson, Alastair H F Kroon, Dick AGE; Continuous flow stable isotope ratio mass spectrometer (IRMS), Elementar Analysensysteme, isoprime precisION; coupled with Gilson autosampler with automated acidification system, heated tray and iso FLOW system; Cyprus; Depth, composite; Eastern Mediterranean; Event label; Foraminifera, planktic δ13C; Foraminifera, planktic δ18O; Isotope ratio mass spectrometer, Thermo, DELTAplus Advantage; Kottaphi_Hill; Lapatza_Hill; LATITUDE; LONGITUDE; Miocene; OUTCROP; Outcrop sample; Oxygen and carbon stable isotopes; Sample ID; Stable isotope; δ13C, carbonate; δ18O, carbonate We present a c. 12 Ma record of oxygen and carbon stable isotopes from the Island of Cyprus to help constrain the nature and extent of Miocene palaeoceanographic changes in the eastern Mediterranean region. Cyprus includes Neogene deep-sea pelagic sedimentary rocks, which are suitable for stable isotope studies. Our composite geochemical record integrates data from the Lower-Upper Miocene succession at Kottaphi Hill along the northern margin of the Troodos ophiolite, and the Upper Miocene succession at Lapatza Hill to the south of the Kyrenia Range. Calcareous nannofossil biostratigraphy reveals that the composite record spans the Miocene Climatic Optimum's onset to the beginning of the Messinian Salinity Crisis. |
| title | δ18O and δ13C stable isotope data from a new composite sediment record, Cyprus (Eastern Mediterranean) |
| topic | AGE; Continuous flow stable isotope ratio mass spectrometer (IRMS), Elementar Analysensysteme, isoprime precisION; coupled with Gilson autosampler with automated acidification system, heated tray and iso FLOW system; Cyprus; Depth, composite; Eastern Mediterranean; Event label; Foraminifera, planktic δ13C; Foraminifera, planktic δ18O; Isotope ratio mass spectrometer, Thermo, DELTAplus Advantage; Kottaphi_Hill; Lapatza_Hill; LATITUDE; LONGITUDE; Miocene; OUTCROP; Outcrop sample; Oxygen and carbon stable isotopes; Sample ID; Stable isotope; δ13C, carbonate; δ18O, carbonate |
| url | https://doi.org/10.1594/PANGAEA.987089 |