H. Behling et al., Late Quaternary vegetational and climate dynamics in northeastern Brazil, inferences from marine core GeoB 3104-1, QUAT SCI R, 19(10), 2000, pp. 981-994
Late Quaternary paleoenvironments from northeastern (NE) Brazil have been s
tudied by pollen analysis of marine sediment. The studied core GeoB 3104-1
(3 degrees 40' S, 37 degrees 43' W, 767 m b.s.l.) from the upper continenta
l slope off NE Brazil is 517 cm long and > 42,000 C-14 yr BP old. Chronolog
ical control was obtained by 12 radiocarbon (AMS) dates from individuals of
the foraminiferal species Globigerinoides sacculifer. Modern pollen analog
s were received from 15 river, lake and forest soil surface samples from NE
Brazil. Marine pollen dates indicate the predominance of semi-arid caating
a vegetation in NE Brazil during the recorded period between > 42,000 and 8
500 C-14 yr BP. The increased fluvial input of terrigenous material, with h
igh concentrations of pollen and specially fern spores, into the marine dep
osits, about 40,000, 33,000 and 24,000 C-14 yr BP and between 15,500 and 11
,800 C-14 yr BP, indicate short-term periods of strong rainfall on the NE B
razilian continent. The expansion of mountain, floodplain and gallery fores
ts characterize the interval between 15,500 and 11,800 C-14 yr BP as the we
ttest recorded period in NE Brazil, which allowed floristic exchanges betwe
en Atlantic rain forest and Amazonian rain forest, and vice versa. The pale
odata from core GeoB 3104-1 confirm the, in general, dry pre-last Glacial M
aximum (LGM) and LGM conditions and the change to wet Lateglacial environme
nts in tropical South America. The annual movement of the intertropical con
vergence zone over NE Brazil, the strong influence of the Antarctic cold fr
onts and changes of the high-pressure cell over the southern Atlantic, may
explain the very wet Lateglacial period in NE Brazil. The documented NE Bra
zilian short-term signals correlate with the documented Dansgaard-Oeschger
cycles and Heinrich events from the northern Hemisphere and suggest strong
teleconnections. (C) 2000 Elsevier Science Ltd. All rights reserved.