Kauri Fossils and Subfossils as a Paleoclimate Data Collection Tool
This Timeline contains Instances of Kauri dendrochronological data (and other paleoclimate data) and the time to which they reference. Each example is placed in time for the time in which that sample died. The timeline operates on the conventional timescale of BCE (Before Common Era); however, each data point is displayed with the timescale of BP (Before Present) which is a timescale measuring times before the reference point of 1950 as time 0. We hope that the magnitude of the kauri paleoclimate record is conveyed through the numerous data points in this timescale. We have included a large number of data points and explained in greater detail events for kauri and specific measurements of kauri paleoclimate data where we felt they were especially important or intersting. The lengths of the three different Milankovitch cycles (zeroed at at the year 2021) along with other interesting events that have occurred during the timeline spanned by kauri paleoclimate data have been included in the timeline to aid in visualizing the scale of the kauri paleoclimate record
KAURI AS A PALEOCLIMATE DATA COLLECTION TOOL
Kauri (Agathis australis) are coniferous trees which have populated the Southern Hemisphere for nearly 20 million years. They are currently native to tropical forests in Australia, New Zealand, Papua New Guinea, New Caledonia and other surrounding regions. Modern Kauri are found in montane forests while the Ancient Kauri are found buried in swamps, preserved in peaty sediment. Researchers believe that Modern Kauri are not found in the same ecological setting as Ancient Kauri because human logging efforts eliminated the low altitude populations. Modern kauri trees are often close to 600 years old with it not being uncommon for them to reach ages of over 1000 years. Kauri trees can act as reliable climate proxies because they are responsive in their growth pattens to changes or stresses in the environment which can be observed in the width of their tree rings. Due to their extensive ages, a single kauri tree’s ring chronologies can span several hundreds or even thousands of years. Kauri also disperse pollen which is easily identifiable in sediments, and when conditions are right, the kauri pollen is well preserved. Despite the crowns of these giant trees reaching impressive heights, their pollen is not widely dispersive and as such the presence of kauri pollen in a stratigraphic section is indicative of living trees in that location at the time of deposition. Preserved fossil or sub-fossil Kauri wood indicates that a tree or population experienced a mortality event. Dendrochronology using Ancient Kauri is a relatively new science and there are wide gaps in the historical database; however, through crossmatching the dendrochronological data of different samples, the puzzle of kauri paleoclimate data can be pieced together slowly. The use of kauri as a paleoclimate record is beneficial for several reasons; however, the fact that kauri is tree which is exclusively native to the southern hemisphere means that it also functions to provide paleoclimate data outside of the northern hemisphere. This helps counter some of the Northern hemisphere bias in data collection (especially within the field of dendrochronology). The kauri paleoclimate records need to continue to be updated and compared against each other in order to maintain and build The data within kauri fossils and subfossils is of incredible detail and as such is an immensely valuable resource for data collection. It is truly amazing how kauri can accurately record information about changes during climate fluctuations, information which has become evermore valuable as we now push forwards into a time of great climate uncertainty.
References:
Boswijk, G., Fowler, A. M., Palmer, J. G., Fenwick, P., Hogg, A., Lorrey, A., & Wunder, J. (2014). The late Holocene Kauri Chronology: Assessing the potential of a 4500-year record for Palaeoclimate Reconstruction. Quaternary Science Reviews, 90, 128–142. https://doi.org/10.1016/j.quascirev.2014.02.022
Boswijk, G., Fowler, A., & Palmer, J. (2005). Hidden histories: Tree-ring analysis of late Holocene swamp kauri, Waikato, New Zealand . In M. Calver (Ed.), A forest conscienceness: Proceedings 6th national conference of the australian forest history Society Inc, 12-17 September 2004, Augusta, Western Australia (pp. 517–525). essay, Millpress.
Boswijk, G., Fowler, A., Lorrey, A., Palmer, J., & Ogden, J. (2006). Extension of the New Zealand kauri (agathis australis) chronology to 1724 BC. The Holocene, 16(2), 188–199. https://doi.org/10.1191/0959683606hl919rp
Cooper, A., & Turney, C. (2020). The adams event, a geomagnetic-driven environmental crisis 42,000 years ago. Paleoenvironment. https://doi.org/10.5194/egusphere-egu2020-12314
D'Costa, D. M., Palmer, J., Hogg, A., Turney, C., Fifield, L. K., & Ogden, J. (2009b). Stratigraphy, pollen and 14c dating of Johnston's Gum Hole, a late quaternary fossil kauri (agathis australis) site, Northland, New Zealand. Journal of Quaternary Science, 24(1), 47–59. https://doi.org/10.1002/jqs.1179
D'Costa, D., Boswijk, G., & Ogden, J. (2009a). Holocene vegetation and environmental reconstructions from swamp deposits in the Dargaville region of the North Island, New Zealand: Implications for the history of Kauri (agathis australis). The Holocene, 19(4), 559–574. https://doi.org/10.1177/0959683609104026
Lorrey, A. M., Boswijk, G., Hogg, A., Palmer, J. G., Turney, C. S. M., Fowler, A. M., Ogden, J., & Woolley, J.-M. (2018). The scientific value and potential of New Zealand Swamp Kauri. Quaternary Science Reviews, 183, 124–139. https://doi.org/10.1016/j.quascirev.2017.12.019
Lorrey, A., & Martin, T. (2005). Use of modern tree-fall patterns as a guideline for interpreting prostrate trees at a pre-last glacial maximum paleoforest site, Upper North Island, New Zealand. Journal of Geophysical Research: Biogeosciences, 110(G2). https://doi.org/10.1029/2005jg000040
Ogden, J., Hogg, A. G., Newham, R. M., Hendy, C., & Wilson, A. (1993). Erratum: The late quaternery history of kauri (agathis australis) in New Zealand and its climatic significance. Journal of Biogeography, 20(6), 706. https://doi.org/10.2307/2845524
Palmer, J. G., Turney, C. S. M., Cook, E. R., Fenwick, P., Thomas, Z., Helle, G., Jones, R., Clement, A., Hogg, A., Southon, J., Bronk Ramsey, C., Staff, R., Muscheler, R., Corrège, T., & Hua, Q. (2016). Changes in El Niño – Southern Oscillation (ENSO) conditions during the Greenland Stadial 1 (GS-1) chronozone revealed by New Zealand tree-rings. Quaternary Science Reviews, 153, 139–155. https://doi.org/10.1016/j.quascirev.2016.10.003
Palmer, J. G., Turney, C. S. M., Hogg, A. G., Lorrey, A. M., & Jones, R. J. (2015). Progress in refining the global radiocarbon calibration curve using New Zealand kauri (agathis australis) tree-ring series from Oxygen Isotope Stage 3. Quaternary Geochronology, 27, 158–163. https://doi.org/10.1016/j.quageo.2015.02.028
Palmer, J., Lorrey, A., Turney, C. S., Hogg, A., Baillie, M., Fifield, K., & Ogden, J. (2006). Extension of New Zealand kauri (agathis australis) tree-ring chronologies into oxygen isotope stage (OIS) 3. Journal of Quaternary Science, 21(7), 779–787. https://doi.org/10.1002/jqs.1075
Turney, C. S. M., Palmer, J., Bronk Ramsey, C., Adolphi, F., Muscheler, R., Hughen, K. A., Staff, R. A., Jones, R. T., Thomas, Z. A., Fogwill, C. J., & Hogg, A. (2016). High-precision dating and correlation of ice, marine and terrestrial sequences spanning Heinrich event 3: Testing mechanisms of interhemispheric change using New Zealand ancient kauri (agathis australis). Quaternary Science Reviews, 137, 126–134. https://doi.org/10.1016/j.quascirev.2016.02.005
Turney, C. S., Fifield, L. K., Palmer, J. G., Hogg, A. G., Baillie, M. G., Galbraith, R., Ogden, J., Lorrey, A., & Tims, S. G. (2007). Towards a radiocarbon calibration for oxygen isotope stage 3 using New Zealand kauri (agathis australis). Radiocarbon, 49(2), 447–457. https://doi.org/10.1017/s0033822200042375
van den Bos, V., Rees, A., Newnham, R., Vandergoes, M., Wilmshurst, J., & Augustinus, P. (2018). Holocene temperature, humidity and seasonality in northern New Zealand linked to southern hemisphere summer insolation. Quaternary Science Reviews, 201, 77–88. https://doi.org/10.1016/j.quascirev.2018.10.008