V
van der Johannes Plicht
Researcher at University of Groningen
Publications - 70
Citations - 3338
van der Johannes Plicht is an academic researcher from University of Groningen. The author has contributed to research in topics: Radiocarbon dating & Holocene. The author has an hindex of 28, co-authored 70 publications receiving 3135 citations.
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Reporting C-14 activities and concentrations
TL;DR: Three modes of reporting (super 14) C activities are in use, in part analogous to the internationally accepted (IAEA) conventions for stable isotopes: (1) absolute activity, the specific activity of a stable isotope or the activity per gram of carbon; (2) activity ratio, the ratio between the absolute activities of a sample and the standard; and (3) relative activity.
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The role of solar forcing upon climate change
B. van Geel,O.M. Raspopov,Hans Renssen,van der Johannes Plicht,V. A. Dergachev,Harro A. J. Meijer +5 more
TL;DR: In this paper, the authors argue that variations in solar activity may have played a significant role in forcing climate changes during the Holocene and the upper part of the last Glacial.
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Evidence from northwest European bogs shows ‘Little Ice Age’ climatic changes driven by variations in solar activity
TL;DR: In this paper, an analysis of both 10 Be and 14 C nuclides has been carried out and it has been shown that production-rate changes during Holocene atmospheric radiocarbon concentrations have been due to variations in solar activity.
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A 40,000-year varve chronology from Lake Suigetsu, Japan: Extension of the 14C calibration curve
TL;DR: This paper performed accelerator mass spectrometric (AMS) 14C measurements on >250 terrestrial macrofossil samples from a 40,000-yr varve sequence from Lake Suigetsu, Japan.
High-resolution records of late Holocene climate change and carbon accumulation in two North-West European ombrotrophic peat bogs
Dmitri Mauquoy,T. Engelkes,M.H.M. Groot,F. Markesteijn,Machiel G. Oudejans,van der Johannes Plicht,B. van Geel +6 more
TL;DR: The peat stratigraphy (plant macrofossils, colorimetric humification, pollen/non-pollen microfossil, carbon/nitrogen ratios) of three replicate cores from a raised peat bog in the UK (Walton Moss) and a single core from an elevated peat bogs in Denmark (Lille Vildmose) were examined in an attempt to investigate the relation between long-term climate change and changes in species composition of the peat-forming vegetation as discussed by the authors.