TY - JOUR
T1 - Vegetation state changes in the course of shrub encroachment in an African savanna since about 1850 CE and their potential drivers
AU - Tabares, Ximena
AU - Zimmermann, Heike
AU - Dietze, Elisabeth
AU - Ratzmann, Gregor
AU - Belz, Lukas
AU - Vieth-Hillebrand, Andrea
AU - Dupont, Lydie
AU - Wilkes, Heinz
AU - Mapani, Benjamin
AU - Herzschuh, Ulrike
N1 - Funding Information:
We are very grateful to Johan Le Roux and Chris Steenkamp from Dantica diving club Windhoek for their assistance in the field. We also thank Sefine Kilinc, Rosemary Shikangalah, Myron Eberle, Sarah Bala, Rabja Popall, and Anke Müllenmeister‐Sawall for the laboratory work. Cathy Jenks is thanked for proofreading. We thank the reviewers for the very helpful remarks. The research was funded by the German Federal Ministry of Education and Research (BMBF) within the framework of the SPACES Project OPTIMASS (FKZ:01LL1302A) and the Initiative and Networking Fund of the Helmholtz Association.
Publisher Copyright:
© 2019 The Authors. Ecology and Evolution published by John Wiley & Sons Ltd.
PY - 2020/1/1
Y1 - 2020/1/1
N2 - Shrub encroachment has far-reaching ecological and economic consequences in many ecosystems worldwide. Yet, compositional changes associated with shrub encroachment are often overlooked despite having important effects on ecosystem functioning. We document the compositional change and potential drivers for a northern Namibian Combretum woodland transitioning into a Terminalia shrubland. We use a multiproxy record (pollen, sedimentary ancient DNA, biomarkers, compound-specific carbon (δ13C) and deuterium (δD) isotopes, bulk carbon isotopes (δ13Corg), grain size, geochemical properties) from Lake Otjikoto at high taxonomical and temporal resolution. We provide evidence that state changes in semiarid environments may occur on a scale of one century and that transitions between stable states can span around 80 years and are characterized by a unique vegetation composition. We demonstrate that the current grass/woody ratio is exceptional for the last 170 years, as supported by n-alkane distributions and the δ13C and δ13Corg records. Comparing vegetation records to environmental proxy data and census data, we infer a complex network of global and local drivers of vegetation change. While our δD record suggests physiological adaptations of woody species to higher atmospheric pCO2 concentration and drought, our vegetation records reflect the impact of broad-scale logging for the mining industry, and the macrocharcoal record suggests a decrease in fire activity associated with the intensification of farming. Impact of selective grazing is reflected by changes in abundance and taxonomical composition of grasses and by an increase of nonpalatable and trampling-resistant taxa. In addition, grain-size and spore records suggest changes in the erodibility of soils because of reduced grass cover. Synthesis. We conclude that transitions to an encroached savanna state are supported by gradual environmental changes induced by management strategies, which affected the resilience of savanna ecosystems. In addition, feedback mechanisms that reflect the interplay between management legacies and climate change maintain the encroached state.
AB - Shrub encroachment has far-reaching ecological and economic consequences in many ecosystems worldwide. Yet, compositional changes associated with shrub encroachment are often overlooked despite having important effects on ecosystem functioning. We document the compositional change and potential drivers for a northern Namibian Combretum woodland transitioning into a Terminalia shrubland. We use a multiproxy record (pollen, sedimentary ancient DNA, biomarkers, compound-specific carbon (δ13C) and deuterium (δD) isotopes, bulk carbon isotopes (δ13Corg), grain size, geochemical properties) from Lake Otjikoto at high taxonomical and temporal resolution. We provide evidence that state changes in semiarid environments may occur on a scale of one century and that transitions between stable states can span around 80 years and are characterized by a unique vegetation composition. We demonstrate that the current grass/woody ratio is exceptional for the last 170 years, as supported by n-alkane distributions and the δ13C and δ13Corg records. Comparing vegetation records to environmental proxy data and census data, we infer a complex network of global and local drivers of vegetation change. While our δD record suggests physiological adaptations of woody species to higher atmospheric pCO2 concentration and drought, our vegetation records reflect the impact of broad-scale logging for the mining industry, and the macrocharcoal record suggests a decrease in fire activity associated with the intensification of farming. Impact of selective grazing is reflected by changes in abundance and taxonomical composition of grasses and by an increase of nonpalatable and trampling-resistant taxa. In addition, grain-size and spore records suggest changes in the erodibility of soils because of reduced grass cover. Synthesis. We conclude that transitions to an encroached savanna state are supported by gradual environmental changes induced by management strategies, which affected the resilience of savanna ecosystems. In addition, feedback mechanisms that reflect the interplay between management legacies and climate change maintain the encroached state.
KW - climate change
KW - fossil pollen
KW - land-use change
KW - savanna ecology
KW - sedaDNA
KW - state and transition
KW - tree–grass interactions
KW - metabarcoding
KW - Vegetation change through time
UR - http://www.scopus.com/inward/record.url?scp=85078510834&partnerID=8YFLogxK
U2 - 10.1002/ece3.5955
DO - 10.1002/ece3.5955
M3 - Article
AN - SCOPUS:85078510834
SN - 2045-7758
VL - 10
SP - 962
EP - 979
JO - Ecology and Evolution
JF - Ecology and Evolution
IS - 2
ER -