Evidence map›Paper›PMID 29773861›Full record

ArticleScientific reports2018

Uncoupling human and climate drivers of late Holocene vegetation change in southern Brazil.

Mark Robinson, Jonas Gregorio De Souza, S Yoshi Maezumi, Macarena Cárdenas, Luiz Pessenda, Keith Prufer, Rafael Corteletti, Deisi Scunderlick, Francis Edward Mayle, Paulo De Blasis and 1 more

Abstract read
In one paragraph

Article in Scientific reports, 2018. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 9 papers.

0numbers the graph read from it
0cells of the map it votes in
9citing papers in PubMed
–field-weighted citation impact
1 · What the graph read from it

What it found

Each row is one number read from the abstract, on the scale the paper reported it, with its interval. Left of the dashed line favours the treatment, right favours the comparator. Under each row is the sentence it came from. New to these charts? A ten-minute tutorial.

The abstract states no effect estimate the extractor could read, or names no intervention and outcome on the map, so this paper lights no cell and moves no belief. It is still indexed, cited and linked below.

2 · The registry

The trial behind it

Trials whose registry record cites this paper, or whose number appears in the abstract. A trial that started after this paper was published is citing it as background, not reporting it.

Neither the registry nor the abstract names a trial number. If this is a trial report, that itself is worth knowing.

3 · Its place in the literature

Who cites it

9 citing papers in PubMed.

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4 · The record

Corrections and comments

PubMed lists nothing against this paper. Absence here is not a guarantee, only a check that was made.

5 · Who and what money

Authors and funding

11 authors.

Mark RobinsonDepartment of Archaeology, University of Exeter, 222 Laver Building, North Park Road, Exeter, Devon, EX4 4QE, UK. markrobinson.uk@gmail.com.
Jonas Gregorio De SouzaDepartment of Archaeology, University of Exeter, 222 Laver Building, North Park Road, Exeter, Devon, EX4 4QE, UK.ORCID 0000-0001-6032-4443
S Yoshi MaezumiDepartment of Archaeology, University of Exeter, 222 Laver Building, North Park Road, Exeter, Devon, EX4 4QE, UK.
Macarena CárdenasCentre for Past Climate Change and Department of Geography & Environmental Science, University of Reading, Reading, RG6 6DW, UK.
Luiz PessendaCentre of Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, 13416-000, Brazil.
Keith PruferDepartment of Anthropology, University of New Mexico, MCS01-1040, Albuquerque, NM, 87106, USA.ORCID 0000-0003-3173-1546
Rafael CortelettiInstituto de Ciências Humanas, Departamento de Antropologia e Arqueologia, Universidade Federal de Pelotas, Rua Cel. Alberto Rosa, 154, Pelotas, RS, Brazil.ORCID 0000-0001-5606-9910
Deisi ScunderlickUniversidade do Sul de Santa Caterina, Av. José Acácio Moreira 787, Bairro Dehon, 88.704-900 - Tubarão, Santa Catarina, Brazil.
Francis Edward MayleCentre of Nuclear Energy in Agriculture, University of São Paulo, Piracicaba, 13416-000, Brazil.
Paulo De BlasisLaboratório de Arqueologia Regional, Museu de Arqueologia e Etnologia, Universidade de São Paulo, São Paulo, Brazil.
José IriarteDepartment of Archaeology, University of Exeter, 222 Laver Building, North Park Road, Exeter, Devon, EX4 4QE, UK.ORCID 0000-0002-8155-5360

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

In the highlands of southern Brazil an anthropogenitcally driven expansion of forest occurred at the expense of grasslands between 1410 and 900 cal BP, coincident with a period of demographic and cultural change in the region. Previous studies have debated the relative contributions of increasing wetter and warmer climate conditions and human landscape modifications to forest expansion, but generally lacked high resoltiuon proxies to measure these effects, or have relied on single proxies to reconstruct both climate and vegetation. Here, we develop and test a model of natural ecosystem distribution against vegetation histories, paleoclimate proxies, and the archaeological record to distinguish human from temperature and precipitation impacts on the distribution and expansion of Araucaria forests during the late Holocene. Carbon isotopes from soil profiles confirm that in spite of climatic fluctuations, vegetation was stable and forests were spatially limited to south-facing slopes in the absence of human inputs. In contrast, forest management strategies for the past 1400 years expanded this economically important forest beyond its natural geographic boundaries in areas of dense pre-Columbian occupation, suggesting that landscape modifications were linked to demographic changes, the effects of which are still visible today.

Indexed as

Climate ChangeEcosystemForestsGrasslandBrazilCarbon IsotopesEnvironmental MonitoringForestryRegression AnalysisCarbon Isotopes

Identifiers

PMID29773861
PMCPMC5958110

What OpenQuestion holds

Textmetadata
LicenceCC BY
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Registered trials

None linked

Read under generation 80e0d062 · epoch 390. Bibliography from PubMed, PubMed Central and OpenAlex; grants from NIH RePORTER; trial links from ClinicalTrials.gov; estimates, votes and beliefs from the OpenQuestion graph.