scholarly journals Did pre-Columbian populations of the Amazonian biome reach carrying capacity during the Late Holocene?

2020 ◽  
Vol 376 (1816) ◽  
pp. 20190715 ◽  
Author(s):  
Manuel Arroyo-Kalin ◽  
Philip Riris

The increasingly better-known archaeological record of the Amazon basin, the Orinoco basin and the Guianas both questions the long-standing premise of a pristine tropical rainforest environment and also provides evidence for major biome-scale cultural and technological transitions prior to European colonization. Associated changes in pre-Columbian human population size and density, however, are poorly known and often estimated on the basis of unreliable assumptions and guesswork. Drawing on recent developments in the aggregate analysis of large radiocarbon databases, here we present and examine different proxies for relative population change between 1050 BC and AD 1500 within this broad region. By using a robust model testing approach, our analyses document that the growth of pre-Columbian human population over the 1700 years prior to European colonization adheres to a logistic model of demographic growth. This suggests that, at an aggregate level, these pre-Columbian populations had potentially reached carrying capacity (however high) before the onset of European colonization. Our analyses also demonstrate that this aggregate scenario shows considerable variability when projected geographically, highlighting significant gaps in archaeological knowledge yet also providing important insights into the resilience of past human food procurement strategies. By offering a new understanding of biome-wide pre-Columbian demographic trends based on empirical evidence, our analysis hopes to unfetter novel perspectives on demic expansions, language diversification trajectories and subsistence intensification processes in the Amazonian biome during the late Holocene. This article is part of the theme issue ‘Cross-disciplinary approaches to prehistoric demography’.

2020 ◽  
Author(s):  
Manuel Arroyo-Kalin ◽  
Philip Riris

The increasingly better-known archaeological record of the Amazon basin, the Orinoco basin, and the Guianas both questions the long-standing premise of a pristine tropical rainforest environment and also provides evidence for major biome-scale cultural and technological transitions prior to European colonisation. Associated changes in pre-Columbian human population size and density, however, are poorly known and often estimated on the basis of unreliable assumptions and guesswork. Drawing on recent developments in the aggregate analysis of large radiocarbon databases, here we present and examine different proxies for relative population change between 1050 BC and AD 1500 within this broad region. By using a robust model-testing approach, our analyses document that the growth of pre-Columbian human population over the 1,700 years prior to European colonisation adheres to a logistic model of demographic growth. This suggests that, at an aggregate level, these pre-Columbian populations had likely reached carrying capacity (however high) before the onset of European colonisation. Our analyses also demonstrate that this aggregate scenario shows considerable variability when projected geographically, which bears on our overall understanding of the resilience of past human food procurement strategies. Lastly, our results provide important insights into pre-Columbian demographic trends and offer novel perspectives on demic expansions, language diversification, and subsistence intensification in the Amazonian biome during the late Holocene.


2021 ◽  
Vol 258 ◽  
pp. 106904
Author(s):  
Benjamin Keenan ◽  
Anic Imfeld ◽  
Kevin Johnston ◽  
Andy Breckenridge ◽  
Yves Gélinas ◽  
...  

2019 ◽  
Vol 46 (15) ◽  
pp. 9013-9022 ◽  
Author(s):  
D. J. Bertassoli ◽  
A. O. Sawakuchi ◽  
C. M. Chiessi ◽  
E. Schefuß ◽  
G. A. Hartmann ◽  
...  

2018 ◽  
Vol 350 (1-2) ◽  
pp. 55-64 ◽  
Author(s):  
Isabel Quintana-Cobo ◽  
Patricia Moreira-Turcq ◽  
Renato C. Cordeiro ◽  
Keila Aniceto ◽  
Alain Crave ◽  
...  

2017 ◽  
Vol 89 (1) ◽  
pp. 75-89 ◽  
Author(s):  
Paula A. Rodríguez-Zorro ◽  
Bruno Turcq ◽  
Renato C. Cordeiro ◽  
Luciane S. Moreira ◽  
Renata L. Costa ◽  
...  

AbstractLocated at the northwestern part of the Amazon basin, Rio Negro is the largest black-water river in the world and is one of the poorest studied regions of the Amazon lowlands. In the middle-upper part of the Rio Negro were retrieved sediment cores form Lake Acarabixi, which were analyzed using pollen, spores, charcoal, and geochemistry. The aim of this study was to detect the influences from humans and river dynamics on the vegetation history in the region. Two main periods of vegetation and river dynamics were detected. From 10,840 to 8240 cal yr BP, the river had a direct influence into the lake. The lake had a regional input of charcoal particles, which reflected the effect of the dry Holocene period in the basin. Furthermore, highland taxa such asHedyosmumandMyrsinewere found at that time along with igapó forest species that are characteristic to tolerate extended flooding likeEschweilera,Macrolobium, Myrtaceae,Swartzia, andAstrocaryum. During the late Holocene (1600 to 650 cal yr BP), more lacustrine phases were observed. There were no drastic changes in vegetation but the presence of pioneer species likeVismiaandCecropia, along with the signal of fires, which pointed to human disturbances.


1996 ◽  
Vol 25 (4) ◽  
pp. 299-300 ◽  
Author(s):  
Kohei Imura ◽  
Ryotarou Midorikawa ◽  
Toshio Kasai ◽  
Hiroshi Ohoyama ◽  
Dock-Chil Che

2015 ◽  
Vol 12 (17) ◽  
pp. 15011-15050 ◽  
Author(s):  
W. Knorr ◽  
L. Jiang ◽  
A. Arneth

Abstract. Wildfires are by far the largest contributor to global biomass burning and constitute a large global source of atmospheric traces gases and aerosols. Such emissions have a considerable impact on air quality and constitute a major health hazard. Biomass burning also influences the radiative balance of the atmosphere and is thus not only of societal, but also of significant scientific interest. There is a common perception that climate change will lead to an increase in emissions as hot and dry weather events that promote wildfire will become more common. However, even though a few studies have found that the inclusion of CO2 fertilization of photosynthesis and changes in human population patterns will tend to somewhat lower predictions of future wildfire emissions, no such study has included full ensemble ranges of both climate predictions and population projections, including the effect of different degrees of urbanisation. Here, we present a series of 124 simulations with the LPJ-GUESS-SIMFIRE global dynamic vegetation – wildfire model, including a semi-empirical formulation for the prediction of burned area based on fire weather, fuel continuity and human population density. The simulations comprise Climate Model Intercomparison Project 5 (CMIP5) climate predictions from eight Earth system models using two Representative Concentration Pathways (RCPs) and five scenarios of future human population density based on the series of Shared Socioeconomic Pathways (SSPs), sensitivity tests for the effect of climate and CO2, as well as a sensitivity analysis using two alternative parameterisations of the semi-empirical burned-area model. Contrary to previous work, we find no clear future trend of global wildfire emissions for the moderate emissions and climate change scenario based on the RCP 4.5. Only historical population change introduces a decline by around 15 % since 1900. Future emissions could either increase for low population growth and fast urbanisation, or continue to decline for high population growth and slow urbanisation. Only for high future climate change (RCP8.5), wildfire emissions start to rise again after ca. 2020 but are unlikely to reach the levels of 1900 by the end of the 21st century. We find that climate warming will generally increase the risk of fire, but that this is only one of several equally important factors driving future levels of wildfire emissions, which include population change, CO2 fertilisation causing woody thickening, increased productivity and fuel load, and faster litter turnover in a warmer climate.


2020 ◽  
Vol 29 (3) ◽  
pp. 431-449
Author(s):  
J. R. Cuthbert

This paper sets out to de-mystify the effects of the Barnett Formula – the mechanism which has delivered the bulk of the funding for Scottish domestic services over the past forty years. There has always been considerable ambiguity about the effects of the formula: with some holding that it is a mechanism which would eventually deliver converging levels of per capita spending in the different countries of the UK: while others held that it protected expenditure differentials. The paper explains why, partly because of the effects of relative population change, both views were correct at different times in the period up to 2015. In particular, at times of austerity, the formula operated to protect relative per capita spending levels in Scotland. Largely by accident, the Barnett Formula delivered some of the features expected in a properly functioning monetary union. After 2015, however, with the introduction of the post referendum fiscal settlement, the position is quite different. While Barnett still plays a part, the overall effect of the new funding system is to place Scotland in a vulnerable position, where it is at much greater risk of falling into a cycle of economic decline relative to the rest of the UK.


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