Holocene paleoclimate inferred from stable isotope (δ18O and δ13C) values in Sphagnum cellulose, Mohos peat bog, Romania
Szerző(k): Túri Marianna; Hubay Katalin; Molnár Mihály; Braun Mihály; László Elemér; Futó István; Palcsu László
Évszám: 2021
Folyóirat/tanulmánykötet: JOURNAL OF PALEOLIMNOLOGY
We measured stable isotopes (d18O and d13C) in Sphagnum cellulose that was extracted from a long peat core drilled in the ombrotrophic Mohos peat bog, Ciomadul Mountain, Romania. The 10-m-long peat profile spans the period from 11,800 cal yr BP to present. The d18O and d13C data indicate there were several cooling events and warm periods in the area of the Mohos peat bog during the Holocene.
Eredeti fellelhetőség: mtmt.hu
