Citation:

Allen, S., M. Sprenger, G. Bowen, AND J. Renee Brooks. Spatial and Temporal Variations in Plant Source Water: O and H Isotope Ratios from Precipitation to Xylem Water. Chapter 18, Stable Isotopes in Tree Rings: Inferring Physiological, Climatic and Environmental Responses. Springer, Heidelberg, Germany, 8:501-535, (2022). https://doi.org/10.1007/978-3-030-92698-4_18

Impact/Purpose:

The stable isotopic composition of tree rings contain detailed physiological and environmental information that provide annual records to past environments and the forest responses to those environments. This chapter is part of a book which provides methods and the background theory for interpreting tree-ring isotopic data. Specifically, this chapter addresses the influence of source water - the varying isotopic compositions of water that trees take up, and the source water influence on the hydrogen and oxygen isotope ratios contained within tree rings.

Description:

The water present within trees when sugars and cellulose are formed is the source of hydrogen and oxygen atoms that are incorporated into tree-ring cellulose (See Chapter 10 and 11). However, the isotope composition of relevant water pools is often unknown when trying to interpret δ18O and δ2H isotopic records in tree rings. This chapter focuses on the factors that can influence the O and H isotope ratios of source waters for trees. Trees generally use water that originated as precipitation, but this does not mean that the isotope ratios of water used by trees – predominantly taken up by roots from soils – and incorporated in cellulose exactly matches precipitation isotope ratios. Precipitation isotope ratios vary in space and time, and only a fraction of all precipitation infiltrates soils, reaches roots, and is ultimately taken up by trees. Considering species, soils, and climates may allow for predicting which fraction of water resides in the root-zone during the growing seasons, and how its isotope ratios deviate from that of average precipitation. Here we provide an overview of the terrestrial water cycle and the associated transport and fractionation processes that influence the stable isotope ratios of water used by trees. We highlight obstacles and opportunities to be considered, towards more accurately interpreting the records of O and H isotope ratios in tree cellulose.

URLs/Downloads:

Record Details: