Results of a case study of landform development and sedimentation in humid
tropical lowland environments on Halmahera island, eastern Indonesia, are p
resented with the aim to better characterise tropical lowland environments
in the context of Late Quaternary environmental change studies. First, the
geologic, morphologic and environmental settings of the two areas, the inte
rior Kao River plain and the Kao coastal zone (N. Halmahera), are presented
. Subsequently, data concerning Late Pleistocene and Holocene landform deve
lopment, sedimentation and coastal processes are discussed. Pleistocene lan
dform development involved volcaniclastic, sedimentation, base levelling of
coastal lowlands, prolonged weathering and crust formation, coastal uplift
and eustatic sea level change. A conspicuous ferricrete crust in the subso
il of the coastal plain is tentatively dated with C-14 AMS analysis and iso
topes of organic matter encapsulated in the soil ferricrete have been deter
mined. Due to interacting sea level change, neotectonic uplift, climatic, h
ydrologic and vegetational change, unequivocal evidence for anomalous Late
Pleistocene or Holocene environmental conditions is difficult to obtain. Du
rin- the Nhd-Late Holocene, a low-energy fluvial systems and swamps existed
in the interior Kao River plain; a dense open swamp/swamp forest vegetatio
n contributed to extremely high sedimentation rates in this depositional ba
sin. Palynological analysis of the organic swamp deposits indicates little
or no change in sedimentary environmental settings and swamp vegetations, a
nd indications for early human presence in the area. In the coastal area ac
cretion and delta progradation occurred after the Early-Mid Holocene format
ion of a marine erosion cliff. Tentative evidence for early human presence
in the Kao area is derived from charcoal particle frequencies in sediments
and the existence of natural grasslands in the coastal zone. As most of the
geologic and environmental characteristics of the tropical lowlands in the
Kao area are common in eastern Indonesia, the study provides useful inform
ation for ongoing research in the region. (C) 2001 Elsevier Science B.V. Al
l rights reserved.