Quantification of termite bioturbation in a savannah ecosystem: application of OSL dating

TY - JOUR

T1 - Quantification of termite bioturbation in a savannah ecosystem: application of OSL dating

AU - Kristensen, Jeppe Ågård

AU - Thomsen, Kristina J.

AU - Murray, Andrew S.

AU - Buylaert, Jan-Pieter

AU - Jain, Mayank

AU - Breuning-Madsen, Henrik

PY - 2015/10/1

Y1 - 2015/10/1

N2 - Luminescence dating is one of the most promising technique available for studying bioturbation on pedological timescales. In this study, we use multi-grain and single-grain quartz OSL to quantify termite bioturbation processes (Macrotermes natalensis) in a savannah ecosystem in Ghana. Termites transport soil from depth to the surface to construct termitaria. Over time, erosion levels these mounds and returns the sediment to the soil surface. These two processes of construction and erosion together represent an upward “conveyor belt” sediment transport process. We find that the sediment is effectively bleached during the erosion process allowing us to quantify retrospectively, for the first time, the surface deposition rate, the inverse of the upwards transport rate. At this site, this is ~0.28 mm year−1 and began about 4.000 years ago. Downward mixing through subsurface galleries may replace 10–20% of the volume ka−1 below the unit formed by reburied termite deposits

AB - Luminescence dating is one of the most promising technique available for studying bioturbation on pedological timescales. In this study, we use multi-grain and single-grain quartz OSL to quantify termite bioturbation processes (Macrotermes natalensis) in a savannah ecosystem in Ghana. Termites transport soil from depth to the surface to construct termitaria. Over time, erosion levels these mounds and returns the sediment to the soil surface. These two processes of construction and erosion together represent an upward “conveyor belt” sediment transport process. We find that the sediment is effectively bleached during the erosion process allowing us to quantify retrospectively, for the first time, the surface deposition rate, the inverse of the upwards transport rate. At this site, this is ~0.28 mm year−1 and began about 4.000 years ago. Downward mixing through subsurface galleries may replace 10–20% of the volume ka−1 below the unit formed by reburied termite deposits

U2 - 10.1016/j.quageo.2015.02.026

DO - 10.1016/j.quageo.2015.02.026

M3 - Journal article

SN - 1871-1014

VL - 30

SP - 334

EP - 341

JO - Quaternary Geochronology

JF - Quaternary Geochronology

ER -