2010
DOI: 10.1130/g31129.1
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Late glacial interhemispheric climate dynamics revealed in South African hyrax middens

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Cited by 88 publications
(57 citation statements)
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“…At Katbakkies, which is within the Fynbos biome and dominated by vegetation using the C 3 photosynthetic pathway, midden d 13 C is interpreted to primarily reflect changes in plant water-use efficiency. Therein, more humid conditions are reflected in more depleted d 13 C values as determined by water availability and temperature (Ehleringer and Cooper, 1988;Pate, 2001;Chase et al, 2011). The absolute values and muted amplitude of the d 13 C record is consistent with changes in water-use efficiency being the primary determinant of d 13 C variability.…”
Section: Stable Isotopesmentioning
confidence: 51%
“…At Katbakkies, which is within the Fynbos biome and dominated by vegetation using the C 3 photosynthetic pathway, midden d 13 C is interpreted to primarily reflect changes in plant water-use efficiency. Therein, more humid conditions are reflected in more depleted d 13 C values as determined by water availability and temperature (Ehleringer and Cooper, 1988;Pate, 2001;Chase et al, 2011). The absolute values and muted amplitude of the d 13 C record is consistent with changes in water-use efficiency being the primary determinant of d 13 C variability.…”
Section: Stable Isotopesmentioning
confidence: 51%
“…The transitions are often characterized by an abruptness that can be explained by mechanisms such as climate-biosphere feedbacks functioning as strong amplifiers of basically moderate trends (Renssen et al, 2006;Castañeda et al, 2009). Apart from orbitally-forced variability, centennial-scale variations such as DansgaardeOeschger cycles, Heinrich events and the Younger Dryas (YD) have also influenced low-latitude climate, although the sign, magnitude and phasing of their impact are debated (Partridge et al, 2004;Brown et al, 2007;Carto et al, 2009;Chase et al, 2011;Stager et al, 2011). Furthermore, Atlantic and Indian Ocean SST changes, related to the thermohaline circulation, are considered to have a strong influence on African climate (Gasse and Van Campo, 1994;deMenocal et al, 2000;Trauth et al, 2010).…”
Section: Long-term Controls On East African Climatementioning
confidence: 99%
“…In hyrax middens, estimates of past changes in water availability have been determined using δ 13 C and δ 15 N (cf. Chase et al, 2011Chase et al, , 2012. For comparison with our pollen record, we use the stable isotope records from the DR2 section of the De Rif midden where the records overlap .…”
Section: Fire History Climate and Vegetation Dynamics At De Rifmentioning
confidence: 99%