Holocene environmental changes in the Central Amazon Basin inferred from Lago Calado (Brazil)
Hermann Behling
Gertrud Keim
Georg Irion
Wolfgang Junk
J. Nunes de Mello
Abstract
Holocene environments have been reconstructed by sedimentological, mineralogical geochemical and high resolution pollen analysis of a 1190 cm-long core from Lago Calado near Manaus in Central Amazonia. The sediment core, dated by eight AMS-radiocarbon dates, has a basal age of
and documents the landscape development from a river valley before 8280 14C yr bp to a lake environment. This change is related to the rise of the Central Amazonian water level, controlled by the postglacial sea-level rise. Pollen analytical results show the formation of a local Mauritia palm-swamp along the river margin between 8280 and 7700 14C yr bp. At that time, highly diverse terra firme (unflooded upland) Amazon rainforest and poorly developed várzea/igapó (inundated) forests along the river characterized the vegetation. The expansion of várzea/igapó forests and a strong presence of aquatic plants started at 7700 14C yr bp, reflecting the rise of the Amazonian water level and the formation of the Lago Calado. The occurrence of abundant Poaceae and Cyperaceae pollen in the lake sediments since 7770 14C yr bp, suggest both the local colonization of unflooded mud banks around the lake margin and the formation of flooding meadows. Open exposed unflooded mud areas, periodically colonized by herbs, are related to seasonal Amazonian high and low water stands. In respect to the abundance of Poaceae pollen during the early and mid Holocene, these open areas must have been large, suggesting brief annual high and extensive annual low Amazonian water stands. After 4070 14C yr bp the proportion of várzea/igapó forest areas was larger than before. Herbs were less abundant, probably due to the smaller area of unflooded mud banks. The Amazonian water levels must have been higher and the period of the annual high water stands was probably longer than before. Since 2080 14C yr bp, the largest proportion of várzea/igapo forests is recorded, reflecting the highest Amazonian water level. Herbs were rare, suggesting that open unflooded mud areas around the lake were relatively small. This may perhaps also indicate that the seasonal period of the Amazonian high water level was the longest since 2080 14C yr bp. The increase of Cecropia, Poaceae and Alternanthera during the last 150 yr, suggests stronger human impact on the local vegetation. Changes to higher Amazonian water levels are related to the rise of the Atlantic sea-level. Relatively short annual high water levels during the early Holocene and relatively long annual high water levels since 4070 and especially since 2080 14C yr bp, can be interpreted as a climate change from a drier early Holocene (with lower annual rainfall rates and longer dry periods) until 4070 14C yr bp to a wetter late Holocene.
Behling H., Keim G., Irion G., Junk W. and Nunes de Mello J. (2001) Holocene environmental changes in the Central Amazon Basin inferred from Lago Calado (Brazil). 173(1-2): 87-101. 10.1016/S0031-0182(01)00321-2
@article{Behling2001,
Title = {Holocene environmental changes in the Central Amazon Basin inferred from Lago Calado (Brazil)},
Author = {Behling, Hermann and Keim, Gertrud and Irion, Georg and Junk, Wolfgang and Nunes de Mello, J.},
Editor = {},
Year = {2001},
Pages = {87-101},
Volume = {173},
Doi = {10.1016/S0031-0182(01)00321-2},
Abstract = {Holocene environments have been reconstructed by sedimentological, mineralogical geochemical and high resolution pollen analysis of a 1190 cm-long core from Lago Calado near Manaus in Central Amazonia. The sediment core, dated by eight AMS-radiocarbon dates, has a basal age of
and documents the landscape development from a river valley before 8280 14C yr bp to a lake environment. This change is related to the rise of the Central Amazonian water level, controlled by the postglacial sea-level rise. Pollen analytical results show the formation of a local Mauritia palm-swamp along the river margin between 8280 and 7700 14C yr bp. At that time, highly diverse terra firme (unflooded upland) Amazon rainforest and poorly developed várzea/igapó (inundated) forests along the river characterized the vegetation. The expansion of várzea/igapó forests and a strong presence of aquatic plants started at 7700 14C yr bp, reflecting the rise of the Amazonian water level and the formation of the Lago Calado. The occurrence of abundant Poaceae and Cyperaceae pollen in the lake sediments since 7770 14C yr bp, suggest both the local colonization of unflooded mud banks around the lake margin and the formation of flooding meadows. Open exposed unflooded mud areas, periodically colonized by herbs, are related to seasonal Amazonian high and low water stands. In respect to the abundance of Poaceae pollen during the early and mid Holocene, these open areas must have been large, suggesting brief annual high and extensive annual low Amazonian water stands. After 4070 14C yr bp the proportion of várzea/igapó forest areas was larger than before. Herbs were less abundant, probably due to the smaller area of unflooded mud banks. The Amazonian water levels must have been higher and the period of the annual high water stands was probably longer than before. Since 2080 14C yr bp, the largest proportion of várzea/igapo forests is recorded, reflecting the highest Amazonian water level. Herbs were rare, suggesting that open unflooded mud areas around the lake were relatively small. This may perhaps also indicate that the seasonal period of the Amazonian high water level was the longest since 2080 14C yr bp. The increase of Cecropia, Poaceae and Alternanthera during the last 150 yr, suggests stronger human impact on the local vegetation. Changes to higher Amazonian water levels are related to the rise of the Atlantic sea-level. Relatively short annual high water levels during the early Holocene and relatively long annual high water levels since 4070 and especially since 2080 14C yr bp, can be interpreted as a climate change from a drier early Holocene (with lower annual rainfall rates and longer dry periods) until 4070 14C yr bp to a wetter late Holocene.},
}
TY - JOUR
AU - Behling, Hermann
AU - Keim, Gertrud
AU - Irion, Georg
AU - Junk, Wolfgang
AU - Nunes de Mello, J.
TI - Holocene environmental changes in the Central Amazon Basin inferred from Lago Calado (Brazil)
PY - 2001
SP - 87-101
VL - 173
DO - 10.1016/S0031-0182(01)00321-2
AB - Holocene environments have been reconstructed by sedimentological, mineralogical geochemical and high resolution pollen analysis of a 1190 cm-long core from Lago Calado near Manaus in Central Amazonia. The sediment core, dated by eight AMS-radiocarbon dates, has a basal age of
and documents the landscape development from a river valley before 8280 14C yr bp to a lake environment. This change is related to the rise of the Central Amazonian water level, controlled by the postglacial sea-level rise. Pollen analytical results show the formation of a local Mauritia palm-swamp along the river margin between 8280 and 7700 14C yr bp. At that time, highly diverse terra firme (unflooded upland) Amazon rainforest and poorly developed várzea/igapó (inundated) forests along the river characterized the vegetation. The expansion of várzea/igapó forests and a strong presence of aquatic plants started at 7700 14C yr bp, reflecting the rise of the Amazonian water level and the formation of the Lago Calado. The occurrence of abundant Poaceae and Cyperaceae pollen in the lake sediments since 7770 14C yr bp, suggest both the local colonization of unflooded mud banks around the lake margin and the formation of flooding meadows. Open exposed unflooded mud areas, periodically colonized by herbs, are related to seasonal Amazonian high and low water stands. In respect to the abundance of Poaceae pollen during the early and mid Holocene, these open areas must have been large, suggesting brief annual high and extensive annual low Amazonian water stands. After 4070 14C yr bp the proportion of várzea/igapó forest areas was larger than before. Herbs were less abundant, probably due to the smaller area of unflooded mud banks. The Amazonian water levels must have been higher and the period of the annual high water stands was probably longer than before. Since 2080 14C yr bp, the largest proportion of várzea/igapo forests is recorded, reflecting the highest Amazonian water level. Herbs were rare, suggesting that open unflooded mud areas around the lake were relatively small. This may perhaps also indicate that the seasonal period of the Amazonian high water level was the longest since 2080 14C yr bp. The increase of Cecropia, Poaceae and Alternanthera during the last 150 yr, suggests stronger human impact on the local vegetation. Changes to higher Amazonian water levels are related to the rise of the Atlantic sea-level. Relatively short annual high water levels during the early Holocene and relatively long annual high water levels since 4070 and especially since 2080 14C yr bp, can be interpreted as a climate change from a drier early Holocene (with lower annual rainfall rates and longer dry periods) until 4070 14C yr bp to a wetter late Holocene.
ER -
