Evidence map›Paper›PMID 27274042›Full record

ArticleProceedings of the National Academy of Sciences of the United States of America2016

Neogene biomarker record of vegetation change in eastern Africa.

Kevin T Uno, Pratigya J Polissar, Kevin E Jackson, Peter B deMenocal

Abstract read
In one paragraph

Article in Proceedings of the National Academy of Sciences of the United States of America, 2016. The graph could read no effect estimate from its abstract, so it casts no vote on the map. Cited by 19 papers.

0numbers the graph read from it
0cells of the map it votes in
19citing 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

19 citing papers in PubMed.

  1. The origin and development of the Miocene northwest African savanna.Proceedings of the National Academy of Sciences of the United States of America · 2026
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  10. Intrataxonomic trends in herbivore enamel δNature ecology & evolution · 2021
    Article
  11. Tectonics, climate and the diversification of the tropical African terrestrial flora and fauna.Biological reviews of the Cambridge Philosophical Society · 2021
    Article
  12. Article
  13. Early hominins evolved within non-analog ecosystems.Proceedings of the National Academy of Sciences of the United States of America · 2019
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  14. Article
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  17. Aridity and hominin environments.Proceedings of the National Academy of Sciences of the United States of America · 2017
    Article
  18. Mio-Pliocene aridity in the south-central Andes associated with Southern Hemisphere cold periods.Proceedings of the National Academy of Sciences of the United States of America · 2017
    Article
  19. Issues in human evolution.Proceedings of the National Academy of Sciences of the United States of America · 2016
    Article
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

4 authors.

Kevin T UnoLamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964; kevinuno1@gmail.com.ORCID 0000-0001-6882-0900
Pratigya J PolissarLamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964;
Kevin E JacksonDepartment of Geology and Environmental Geosciences, Lafayette College, Easton, PA 18042;
Peter B deMenocalLamont-Doherty Earth Observatory of Columbia University, Palisades, NY 10964; Department of Earth and Environmental Sciences, Columbia University, New York, NY 10027.

Funding

No grant is acknowledged in the PubMed record.

6 · The paper itself

Abstract

The evolution of C4 grassland ecosystems in eastern Africa has been intensely studied because of the potential influence of vegetation on mammalian evolution, including that of our own lineage, hominins. Although a handful of sparse vegetation records exists from middle and early Miocene terrestrial fossil sites, there is no comprehensive record of vegetation through the Neogene. Here we present a vegetation record spanning the Neogene and Quaternary Periods that documents the appearance and subsequent expansion of C4 grasslands in eastern Africa. Carbon isotope ratios from terrestrial plant wax biomarkers deposited in marine sediments indicate constant C3 vegetation from ∼24 Ma to 10 Ma, when C4 grasses first appeared. From this time forward, C4 vegetation increases monotonically to present, with a coherent signal between marine core sites located in the Somali Basin and the Red Sea. The response of mammalian herbivores to the appearance of C4 grasses at 10 Ma is immediate, as evidenced from existing records of mammalian diets from isotopic analyses of tooth enamel. The expansion of C4 vegetation in eastern Africa is broadly mirrored by increasing proportions of C4-based foods in hominin diets, beginning at 3.8 Ma in Australopithecus and, slightly later, Kenyanthropus This continues into the late Pleistocene in Paranthropus, whereas Homo maintains a flexible diet. The biomarker vegetation record suggests the increase in open, C4 grassland ecosystems over the last 10 Ma may have operated as a selection pressure for traits and behaviors in Homo such as bipedalism, flexible diets, and complex social structure.

Indexed as

Biological EvolutionGrasslandAfrica, EasternAlkanesBiomarkersCarbon IsotopesPaleontologyPoaceaeAlkanesBiomarkersCarbon Isotopescarbon isotopehomininleaf waxmammalian evolutionmolecular distribution

Identifiers

PMID27274042
PMCPMC4988583

What OpenQuestion holds

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Registered trials

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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.