Late Quaternary vegetation, biodiversity and fire dynamics on the southern Brazilian highland and their implication for conservation and management of modern Araucaria forest and grassland ecosystems
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Late Quaternary vegetation, biodiversity and fire dynamics on
the southern Brazilian highland and their implication for
conservation and management of modern Araucaria forest and
grassland ecosystems
Hermann Behling and Valério DePatta Pillar
Phil. Trans. R. Soc. B 2007 362, doi: 10.1098/rstb.2006.1984, published 28 February 2007
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Phil. Trans. R. Soc. B (2007) 362, 243–251
doi:10.1098/rstb.2006.1984
Published online 19 December 2006
Late Quaternary vegetation, biodiversity and fire
dynamics on the southern Brazilian highland
and their implication for conservation and
management of modern Araucaria forest
and grassland ecosystems
Hermann Behling1,* and Valério DePatta Pillar2
1
Albrecht-von-Haller-Institut für Pflanzenwissenschaften, Georg-August-Universität Göttingen,
Abteilung für Palynologie und Klimadynamik, Untere Karspüle 2, 37073 Göttingen, Germany
2
Departamento de Ecologia, Universidade Federal do Rio Grande do Sul,
CEP 91540-000 Porto Alegre, Brazil
Palaeoecological background information is needed for management and conservation of the highly
diverse mosaic of Araucaria forest and Campos (grassland) in southern Brazil. Questions on the
origin of Araucaria forest and grasslands; its development, dynamic and stability; its response to
environmental change such as climate; and the role of human impact are essential. Further questions
on its natural stage of vegetation or its alteration by pre- and post-Columbian anthropogenic activity
are also important. To answer these questions, palaeoecological and palaeoenvironmental data based
on pollen, charcoal and multivariate data analysis of radiocarbon dated sedimentary archives from
southern Brazil are used to provide an insight into past vegetation changes, which allows us to
improve our understanding of the modern vegetation and to develop conservation and management
strategies for the strongly affected ecosystems in southern Brazil.
Keywords: Late Quaternary; Araucaria forest; Campos (grassland); palaeoecology; conservation;
management
Abbreviations: AD, Anno Domini; cal yr BP, calibrated radiocarbon years before present;
uncal yr BP, uncalibrated radiocarbon years before present
1. INTRODUCTION
Several Neotropical regions harbour the most biodiverse ecosystems on Earth, yet we know only little
about why they are so biodiverse. We are especially
ignorant of the role that history has played in the
development of these hotspots of species richness
including endemism (Churchill et al. 1995, Broecker
1997). This problem is particularly acute in the extraAndean ranges of eastern Brazil, the so-called ‘Mata
Atlantica biodiversity hotspot’, where rigorous palaeoecological work has only begun during the last few years.
In this paper, we present data from the southern
Brazilian highland region, where a mosaic of Campos
(grassland) and Araucaria forests is found. The
presence of these mosaics under modern wet climatic
conditions favourable for forest development has
puzzled naturalists and ecologists for a long time.
Lindman, travelling across southern Brazil in the late
nineteenth century, observed that forests should be
able to expand over these grasslands, and attributed
their presence to the transitional situation between
* Author for
goettingen.de).
correspondence
tropical forests to the north and temperate grasslands
to the south (Lindman 1906). In addition, Rambo
(1956a,b) and Klein (1975, 1984), hypothesized based
primarily on plant geographical evidence, that the
grasslands were the older vegetation type, with forest
expansion being a more recent process after changes to
the more humid climate conditions. Also Hueck (1966)
raised the question of how the southern Brazilian
grassland can exist under the present humid forest
climatic conditions.
Understanding the origin of the grasslands is of prime
importance to their conservation. If the grasslands are as
a consequence of human-induced deforestation,
vegetation management would probably be focused on
re-establishment of forest vegetation. If, however, the
grasslands have prevailed in the past due to different
climatic regimes, it could be reasonable to conserve these
‘natural’ relicts and their high biodiversity.
Sustainable management and conservation of the
modern mosaics of Campos and Araucaria forest
depends, in part, therefore on the determination of
historical reference conditions for the past human
impact, e.g. fire magnitude and frequency, and the
applied use of this information in developing long-term
management and monitoring plans. In this study, we
present the results from a palaeoecological study (fossil
pollen and microfossil charcoal) of a sediment core
(-
One contribution of 14 to a Theme Issue ‘Biodiversity hotspots
through time: using the past to manage the future’.
243
q 2006 The Royal Society
Downloaded from rstb.royalsocietypublishing.org on October 30, 2014
244
H. Behling & V. D. P. Pillar Biodiversity on southern Brazilian highland
20˚
Rio de Janeiro
6
25˚
5
3
7
2
4
Atlantic Ocean
X
1
Porto Alegre
30˚
100 km
55˚
50˚
45˚
Figure 1. Map showing the distribution of Araucaria forest
and Campos in southern Brazil (adapted after Hueck 1953,
1966) and the location of Cambará do Sul (X) and other sites
mentioned in the text: (1) Aparados da Serra, (2) São
Francisco de Paula, (3) Serra do Rio Rastro, (4) Morro da
Igreja, (5) Serra da Boa Vista, (6) Serra Campos Gerais and
(7) São Francisco de Assis.
sampled at Cambará do Sul on the southern Brazilian
highland (Behling et al. 2004) to analyse past vegetation
and fire dynamics. Special emphasis is placed on past
plant diversity dynamics, in order to provide essential
information for management and conservation of this
biodiverse region. Important questions to be addressed
include the following. How natural is the diverse
mosaic of forest and grassland vegetation in southern
Brazil? Was its development caused by pre-Columbian
slash and burn activity, and deforestation of the postColumbian settlers or rather a natural process of
climate-driven forest expansion constrained by grassland fires? Are fires natural or of anthropogenic origin?
What is the effect of climate change, fire and human
impact on the overall biodiversity of the region through
the time? How should we manage and conserve the
modern species-rich forest and grassland ecosystems?
2. (...truncated)