Palynological investigations on vegetation and climate change in the Late Quaternary of Lake Rukche area, Gorkha Himal, Central Nepal

• Published in: Vegetation history and archaeobotany Vol. 13; no. 2; pp. 81 - 90
• Main Authors: Schlütz, Frank, Zech, Wolfgang
• Format: Journal Article
• Language: English
• Published: Heidelberg Springer 01.06.2004; Springer Nature B.V
• Subjects: Anthropogenic factors; Biodiversity; Biomarkers; Charcoal; Climate change; Cloud forests; Communities; Coniferous forests; Data points; Deciduous forests; Environmental studies; Flora; Forest resources; Forests; Glacial lakes; Holocene; Human influences; Humid climates; Hydrologic data; Isotopes; Lakes; Lignin; Meadows; Methodology and general studies; Natural vegetation; Paleoclimatology; Palynology; Pine trees; Pinus roxburghii; Pleistocene; Poaceae; Pollen; Precipitation; Prehistory and protohistory; Quaternary; Rainfall; Sandy soils; Soil stabilization; Spring (season); Stable isotopes; Steppes; Taxa; Vegetation; Vegetation cover; Winter; New; Asia; Nepal; Clearing; Palynology; Breeding; Quaternary; Laboratory; History; Subatlantic; Pollen analysis; Pedology; Vegetation; Environment; Evolution; Forest; Palaeobotany; Reconstitution; Chronology; Dating; Holocene; Isotope Analysis; Pleistocene
• ISSN: 0939-6314; 1617-6278
• DOI: 10.1007/s00334-004-0035-x

Palynological data and pedological investigations including stable isotopes and lignin biomarkers (Glaser et al. in press) from a 4 m core of Lake Rukche (3500 m a.s.l.) enhance our palaeoecological knowledge of the time since the LGM in the Gorkha Himal, Central Nepal. Even before 15000 B.P. forest types became established which prove the existence in Central Nepal of a temperate-humid climate with a considerable amount of winter and spring precipitation from westerly disturbances. Lignin input and pollen data point to a patchy vegetation cover around Lake Rukche with meadow-steppes dominated by Poaceae. Around 15000 B.P. Quercus and Pinus roxburghii dominated the lower altitudes while the vegetation around Lake Rukche was more steppe-like (Chenopodiaceae, Artemisia). Subsequently the climate became warmer and drier as winter and spring precipitation decreased while summer rain remained low. Later on more resource-demanding forests became established under improved temperature and precipitation conditions (Engelhardia). Around Lake Rukche coniferous forests (Abies, Picea) occurred beside meadow-steppes. The transition from the Pleistocene to the Holocene is not recorded. In the Holocene alpine Kobresia-meadows stabilised the soil surface causing sand accumulation to end. During the mid-Holocene (7800—2750 B.P.) humid oak forests with demanding elements (Ilex, Coriaria, Myrsine and Engelhardia) dominated the vegetation cover. A charcoal layer and a marked emergence of fire-induced communities with Pinus roxburghii, Poaceae, Ericaceae and Pteridium are proofs of a first strong anthropogenic change in vegetation which coincided with the climatic deterioration at the onset of the Subatlantic. Since 900 B.P. grazing pressure and the frequency of fires increased, resulting in a replacement of Betula utilis-forests by meadows and woods of Juniperus and Rhododendron. While previous anthropogenic influence increased the biodiversity by promoting replacement communities, recent developments have led to a decrease in biodiversity through loss of natural vegetation communities.