Amazonia and the Anthropocene: What was the spatial extent and intensity of human landscape modification in the Amazon Basin at the end of prehistory?

The Holocene ◽  
2015 ◽  
Vol 25 (10) ◽  
pp. 1588-1597 ◽  
Author(s):  
Dolores R Piperno ◽  
Crystal McMichael ◽  
Mark B Bush
Author(s):  
Jonas Gregorio de Souza

Continuing advances in the archaeology of the Amazon have changed long-standing misconceptions about the rainforest as a homogeneous, nearly pristine environment occupied by small, scattered groups. Massive archaeological sites, deep deposits of anthropogenic soils, and earthworks found over thousands of kilometers now testify to the scale and intensity of past human impact in some parts of the Amazon. However, debate persists about the extent of such transformations, as distinct environments within the Amazon Basin (floodplains, savannas, seasonal forests) reveal different scales and intensities of pre-Columbian landscape modification. In that context, the discovery of hundreds of geometric earthen enclosures in the southern rim of the Amazon is proving that some areas that were previously considered virtually untouched forest may have been densely settled in the past. Although regional variations exist, most southern Amazonian enclosures appear to be defensive earthworks built at the turn of the second millennium ce, a period recognized by archaeologists as one of escalating population densities, migrations, and warfare across the Amazon Basin.


2004 ◽  
Vol 359 (1443) ◽  
pp. 499-514 ◽  
Author(s):  
Francis E. Mayle ◽  
David J. Beerling ◽  
William D. Gosling ◽  
Mark B. Bush

The aims of this paper are to review previously published palaeovegetation and independent palaeoclimatic datasets together with new results we present from dynamic vegetation model simulations and modern pollen rain studies to: (i) determine the responses of Amazonian ecosystems to changes in temperature, precipitation and atmospheric CO 2 concentrations that occurred since the Last Glacial Maximum (LGM), ca . 21 000 years ago; and (ii) use this long–term perspective to predict the likely vegetation responses to future climate change. Amazonia remained predominantly forested at the LGM, although the combination of reduced temperatures, precipitation and atmospheric CO 2 concentrations resulted in forests structurally and floristically quite different from those of today. Cold–adapted Andean taxa mixed with rainforest taxa in central areas, while dry forest species and lianas probably became important in the more seasonal southern Amazon forests and savannahs expanded at forest–savannah ecotones. Net primary productivity (NPP) and canopy density were significantly lower than today. Evergreen rainforest distribution and NPP increased during the glacial—Holocene transition owing to ameliorating climatic and CO 2 conditions. However, reduced precipitation in the Early–Mid–Holocene ( ca . 8000–3600 years ago) caused widespread, frequent fires in seasonal southern Amazonia, causing increased abundance of drought–tolerant dry forest taxa and savannahs in ecotonal areas. Rainforests expanded once more in the Late Holocene owing to increased precipitation caused by greater austral summer insolation, although some of this forest expansion (e.g. in parts of the Bolivian Beni) is clearly caused by palaeo Indian landscape modification. The plant communities that existed during the Early–Mid–Holocene may provide insights into the kinds of vegetation response expected from similar increases in temperature and aridity predicted for the twenty–first century. We infer that ecotonal areas near the margins of the Amazon Basin are liable to be most sensitive to future environmental change and should therefore be targeted with conservation strategies that allow ‘natural’ species movements and plant community re–assortments to occur.


Author(s):  
Vincent Gauci ◽  
Viviane Figueiredo ◽  
Nicola Gedney ◽  
Sunitha Rao Pangala ◽  
Tainá Stauffer ◽  
...  

Inundation-adapted trees were recently established as the dominant egress pathway for soil-produced methane (CH 4 ) in forested wetlands. This raises the possibility that CH 4 produced deep within the soil column can vent to the atmosphere via tree roots even when the water table (WT) is below the surface. If correct, this would challenge modelling efforts where inundation often defines the spatial extent of ecosystem CH 4 production and emission. Here, we examine CH 4 exchange on tree, soil and aquatic surfaces in forest experiencing a dynamic WT at three floodplain locations spanning the Amazon basin at four hydrologically distinct times from April 2017 to January 2018. Tree stem emissions were orders of magnitude larger than from soil or aquatic surface emissions and exhibited a strong relationship to WT depth below the surface (less than 0). We estimate that Amazon riparian floodplain margins with a WT < 0 contribute 2.2–3.6 Tg CH 4  yr −1 to the atmosphere in addition to inundated tree emissions of approximately 12.7–21.1 Tg CH 4  yr −1 . Applying our approach to all tropical wetland broad-leaf trees yields an estimated non-flooded floodplain tree flux of 6.4 Tg CH 4  yr −1 which, at 17% of the flooded tropical tree flux of approximately 37.1 Tg CH 4  yr −1 , demonstrates the importance of these ecosystems in extending the effective CH 4 emitting area beyond flooded lands. This article is part of a discussion meeting issue 'Rising methane: is warming feeding warming? (part 2)'.


2020 ◽  
Author(s):  
Phillip Papastefanou ◽  
Christian S. Zang ◽  
Zlatan Angelov ◽  
Aline Anderson de Castro ◽  
Juan Carlos Jimenez ◽  
...  

Abstract. Over the last decades, the Amazon rainforest was hit by multiple severe drought events. Here we assess the severity and spatial extent of the extreme drought years 2005, 2010, and 2015/2016 in the Amazon region and their impacts on the carbon cycle. As an indicator of drought stress in the Amazon rainforest, we use the widely applied maximum cumulative water deficit (ΔMCWD). Evaluating an ensemble of ten state-of-the-art precipitation datasets for the Amazon region, we find that the spatial extent of the drought in 2005 ranges from 2.8 to 4.2 (mean = 3.2) million km2 (46–71 % of the Amazon basin, mean = 53 %) where ΔMCWD indicates at least moderate drought conditions (ΔMCWD anomaly


2021 ◽  
Author(s):  
Sarah J. Ivory ◽  
Kenneth L. Cole ◽  
R. Scott Anderson ◽  
Andrew Anderson ◽  
Joy McCorriston ◽  
...  

Author(s):  
B.R. FORSBERG, ◽  
M. GASTIL, ◽  
S.K. HAMILTON, ◽  
L.L. HESS, ◽  
I.B.T. LIMA, ◽  
...  
Keyword(s):  

Sign in / Sign up

Export Citation Format

Share Document