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Publications

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Yokoyama Y, Tims S, Froehlich M, Hirabayashi S, Aze T, Fifield LK,…
Nature Scientific Reports
2022
Pinke Z, Decsi B, Jámbor A, Kardos MK, Kern Z, Kozma Z and Ács T
Scientific Reports
2022
DeLong K, Atwood A, Moore A and Sanchez S
Eos
2022
Wan Q, Huang K, Zhang X, Yue Y, Peng H, Yang X and Zheng Z
Quaternary International
2022
Wan et al. 2022: Fig. 1
Daltona AS, Pico T, Gowan EJ, Clague JJ, Forman SL, McMartin I,…
Global and Planetary Change
2022
Fig. 1 Dalton et al. May 2022
Agiadi K, Nawrot R, Albano PG, Koskeridou E and Zuschin M
Environmental Biology of Fishes
2022
Figure 1: Potential and limitations of applying the mean temperature approach to fossil otolith assemblages
Githumbi E, Fyfe R, Gaillard M-J, Trondman A-K, Mazier F, Nielsen A-B…
Earth System Science Data
2022
Githumbi 2022
Dalton AS, Gowan EJ, Mangerud J, Möller P, Lunkka JP and Astakhov V
Earth System Science Data
2022
Hill AC, Whitehouse N, Madella M, Morrison KD and Gaillard M-J
Past Global Changes Magazine
2022
Austermann J and Simms A
Past Global Changes Magazine
2022
PAGES Magazine articles
Agiadi K, Caswell BA, Bas M, Holm P and Lueders-Dumont JA
Past Global Changes Magazine
2022
Garrett E, Gehrels WR, Hayward BW, Newnham R, Gehrels MJ, Morey CJ…
Journal of Quaternary Science
2022
Location of the tidal marsh at Mokomoko Inlet. In panels a and b, tide-gauge station abbreviations are as follows: PWB: Puysegur Welcome Bay, DUN: Dunedin, BLF: Bluff. Panel b shows locations of Mokomoko Inlet (this study), Waikawa Harbour (Figueira, 2012; Figueira and Hayward, 2014), and Pounawea (Southall et al., 2006; Gehrels et al., 2008). Aerial photo of Mokomoko Inlet in panel c is from Bing Maps (https://www.bing.com/maps, image copyright DigitalGlobe, 2020). Panels d and e show the topography and ve
Githumbi E, Pirzamanbein B, Lindström J, Poska A, Fyfe R, Mazier F,…
Frontiers in Ecology and Evolution
2022
Figure 3. Validation datasets of major land-cover types (LCTs: B, broad-leaved forest; C, coniferous forest; O, open land), area of confidence region (CR) and compositional distance (CD) estimates. (A) CR (100 BP–present): area of confidence regions for 100 BP–present time-window (smaller values are better, see Figure 2 for examples of CRs); (B) 100 BP–present: reconstructed proportions of LCTs in Europe for the most recent time window; (C) EFI-FM: observed modern LCT proportions according to the European f
Strandberg G, Lindstrom J, Poska A, Zhang Q, Fyfe R, Githumbi E,…
Quaternary Science Reviews
2022
Fig. 1. Description of the model chain for 6 ka. All RCM simulations read boundary conditions from EC-Earth. A first set of simulations are made with current land cover (0), these climate scenarios are used in LPJ-GUESS to provide the 6 ka potential natural land cover (L1, L2) subsequently used in the RCMs. A Bayesian spatial model is used to reconstruct 6 ka land cover (R) that is also used in the RCMs.
Walker JS, Kopp RE, Little CM & Horton BP
Nature Communications
2022
 Fig. 2: Spatial variability in the time of emergence of modern rates of relative sea level.
Mariani M, Connor SE, Theuerkauf M, Herbert A, Kuneš P, Bowman D,…
Frontiers in Ecology and the Environment
2022
Mariani M, Connor SE, Theuerkauf M, Herbert A, Kuneš P, Bowman D,…
Frontiers in Ecology and the Environment
2022
Img 1: Disruption of cultural burning promotes shrub encroachment and unprecedented wildfires
Gaillard M-J, Githumbi E, Achoundong G, Lézine A-M, Hély C, Lebamba J…
2021
Keogh ME, Törnqvist TE, Kolker AS, Erkens G, Bridgeman JG
Journal of Geophysical Research: Earth Surface
2021
Cerrone C, Vacchi M, Fontana A & Rovere A
Earth System Science Data
2021
Last Interglacial sea-level proxies in the western Mediterranean