Relationships between calibrated ages and depth in stratigraphical sequences: an estimation procedure by mixed-effect regression
By E. Heegaard, Harry John Betteley Birks, R. Telford. 2005
297 citations recorded by the source corpus.
Subfields: Atmospheric Science, Earth-Surface Processes, Paleontology
How researchers see this paper
The researchers whose trusted networks rank it highest, strongest advocate first. Every researcher gets a different order.
In Atmospheric Science
- C. Ramsey
- D. Scholz
- D. Hoffmann
- M. Blaauw
- E. Heegaard
- Manfred Mudelsee
- Kristín Björg Ólafsdóttir
- Michael Schulz
In Earth-Surface Processes
In Paleontology
Citations in the corpus
- Trend analysis of climate time series: A review of methods (2019, background): “…Bennett (1994); Agrinier et al. (1999); Bennett and Fuller (2002); Buck and Millard (2004); Drysdale et al. (2004); Blaauw and Christen (2005); Heegaard et al. (2005); Spötl et al. (2006); Haslett and Parnell (2008); Blaauw (2010); Klauenberg et al. (2011); Scholz and Hoffmann (2011); Blaauw…”
- Estimation of Age-Depth Relationships (2012, background): “In very rare cases, there may be a relationship between age and the between-object variance, perhaps because of increasing displacements with increasing depth (Heegaard et al. 2005).”
- StalAge – An algorithm designed for construction of speleothem age models (2011, methodology): “Heegaard et al. (2005) presented a mixed-effect regression model for 14C-age modelling, which combines the uncertainty of the individual calibrated ages (within-object variance) with an estimation of the variability of the calibrated age distribution as a whole (betweenobject variance).”
- Methods and code for 'classical' age-modelling of radiocarbon sequences. (2010, methodology): “Heegaard et al. (2005) applied mixed-effects modelling, but assumed that calibrated 14C ages can be approximated by a simpler statistical distribution (e.g., Gaussian).”
- BAYESIAN ANALYSIS OF RADIOCARBON DATES (2009, methodology): “Other methods (sometimes not Bayesian) allow for non-linear deposition rates (Christen et al. 1995; Walker et al. 2003; Telford et al. 2004; Heegaard et al. 2005).”