THE DETERMINATION OF LATE QUATERNARY PALEOENVIRONMENTS AT EQUUS CAVE,SOUTH-AFRICA, USING STABLE ISOTOPES AND AMINO-ACID RACEMIZATION IN OSTRICH EGGSHELL
Bj. Johnson et al., THE DETERMINATION OF LATE QUATERNARY PALEOENVIRONMENTS AT EQUUS CAVE,SOUTH-AFRICA, USING STABLE ISOTOPES AND AMINO-ACID RACEMIZATION IN OSTRICH EGGSHELL, Palaeogeography, palaeoclimatology, palaeoecology, 136(1-4), 1997, pp. 121-137
The stable carbon and nitrogen isotopes from organic compounds, and st
able oxygen and carbon isotopes from inorganic carbonate in modern and
fossil ostrich eggshell (OES) at Equus Cave, South Africa, were used
to determine relative changes in C-3 and C-4 vegetation, rainfall, and
temperature throughout the last 17 ka. Amino acid racemization and th
ree new radiocarbon dates were used to assign ages to the individual O
ES fragments analyzed for stable isotopes, and to evaluate the stratig
raphic integrity of the samples. The amino acid racemization and radio
carbon data indicate that most of the OES fragments are not in correct
stratigraphic context, and may have been upwardly and downwardly mixe
d; thus, each fragment was placed in chronological sequence using radi
ocarbon-calibrated amino acid racemization. The stable carbon isotope
data from the fossil OES do not change systematically through the last
17 ka. The ostriches primarily consumed C-3 plants (between 70% and 9
0%), and smaller quantities of C-4 plants (between 30% and 10%), indic
ating that a mixture of C-3 and C-4 plants has been in the vicinity of
Equus Cave for the last 17 ka. Stable nitrogen isotope data from OES
indicate that at 17 ka, mean annual precipitation (MAP) was at a minim
um (190 +/- 50 mm/yr), increased steadily to modern values by 6 ka (60
0 +/- 150 mm/yr), and remained relatively unchanged until present. Sta
ble oxygen isotope data coupled with nitrogen isotope data indicate th
at paleotemperatures were at a minimum between 14 and 17 ka, and reach
ed their maximum in the latest Holocene. This study demonstrates the p
lethora of paleoenvironmental information that can be derived from ana
lysis of three different stable isotopes (carbon, nitrogen, and oxygen
) in the same sample-type (OES), and presents a new tool with wide app
licability for reconstructing paleoenvironments in semi-arid and arid
regions of Africa. (C) 1997 Elsevier Science B.V.