Carbon storage in Amazonia during the last glacial maximum: secondary data and uncertainties.

Abstract:

:The Amazonian forest is, due to its great size, carbon storage capacity and present-day variability in carbon uptake and release, an important component of the global carbon cycle. Paleo-environmental reconstruction is difficult for Amazonia due to the scarcity of primary palynological data and the mis-interpretation of some secondary data. Studies of lacustrine sediment records have shown that Amazonia has known periods in which the climate was drier than it is today. However, not all geomorphological features such as dunes, and slope erosion, which are thought to indicate rainforest regression, date from the time of the Late Glacial Maximum (LGM) and these features do not necessarily correspond to episodes of forest regression. There is also uncertainty concerning LGM carbon storage due to rainforest soils and biomass estimates. Soil carbon content may decrease moderately during the LGM, whereas rainforest biomass may change considerably in response to changes in the global environment. Biomass per unit area in Amazonia has probably been reduced by the cumulative effects of low CO2 concentration, a drier climate and lower temperatures. As few paleo-vegetation data are available, there is considerable uncertainty concerning the amount of carbon stored in Amazonia during the LGM, which may have corresponded to 44-94% of the carbon currently stored in biomass and soils.

journal_name

Chemosphere

journal_title

Chemosphere

authors

Turcq B,Cordeiro RC,Sifeddine A,Simões Filho FF,Albuquerque AL,Abrão JJ

doi

10.1016/s0045-6535(02)00383-1

subject

Has Abstract

pub_date

2002-12-01 00:00:00

pages

821-35

issue

8

eissn

0045-6535

issn

1879-1298

pii

S0045-6535(02)00383-1

journal_volume

49

pub_type

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