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The oldest fossil mushroom

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A new fossil mushroom is described and illustrated from the Lower Cretaceous Crato Formation of northeast Brazil. Gondwanagaricites magnificus gen. et sp. nov. is remarkable for its exceptional preservation as a mineralized replacement in laminated limestone, as all other fossil mushrooms are known from amber inclusions. Gondwanagaricites represents the oldest fossil mushroom to date and the first fossil mushroom from Gondwana.
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RESEARCH ARTICLE
The oldest fossil mushroom
Sam W. Heads
1
*, Andrew N. Miller
1
, J. Leland Crane
1
, M. Jared Thomas
1
, Danielle
M. Ruffatto
1
, Andrew S. Methven
2
, Daniel B. Raudabaugh
1,3
, Yinan Wang
4
1Illinois Natural History Survey, Prairie Research Institute, University of Illinois at Urbana-Champaign,
Champaign, Illinois, United States of America, 2Department of Biology, Savannah State University,
Savannah, Georgia, United States of America, 3Department of Plant Biology, University of Illinois at Urbana-
Champaign, Urbana, Illinois, United States of America, 4Independent Researcher, Arlington, Virginia, United
States of America
*swheads@illinois.edu
Abstract
A new fossil mushroom is described and illustrated from the Lower Cretaceous Crato For-
mation of northeast Brazil. Gondwanagaricites magnificus gen. et sp. nov. is remarkable for
its exceptional preservation as a mineralized replacement in laminated limestone, as all
other fossil mushrooms are known from amber inclusions. Gondwanagaricites represents
the oldest fossil mushroom to date and the first fossil mushroom from Gondwana.
Introduction
Exceptionally preserved fossils can shed important and unprecedented light on the history of
life. Particularly remarkable deposits, known as Lagersta¨tten, yield fossils characterized by
preservation of soft tissues that decay rapidly and which are not normally preserved. In many
cases, large and important groups of soft-bodied organisms would be missing entirely from
the fossil record if not for their exceptional preservation in Lagersta¨tten. Mushrooms, an
ecologically important group of fungi in the order Agaricales, produce fleshy, gilled fruiting
bodies (called basidiomes) that are rarely fossilized [1]. While certainly ancient, they have an
extremely depauperate fossil record with only ten fossil mushrooms reported to date, all
unique amber inclusions ranging from mid-Cretaceous to Early Miocene in age [28]. Here
we report the discovery of a new fossil mushroom that is unique in its preservation as a miner-
alized replacement, and the oldest yet encountered. The specimen comes from the laminated
limestones of the Crato Formation, which outcrop on the northern flanks of the Chapada do
Araripe in Ceara
´, Brazil; a Lagersta¨tte famous for the exceptional preservation of its diverse
Lower Cretaceous paleobiota [911].
Material and methods
The specimen comprises a single, nearly complete mushroom preserved as a primarily goethi-
tic replacement on a small slab (approximately 50 ×60 mm) of typical, buff-colored, millime-
trically-laminated limestone from the Nova Olinda Member; the lowermost unit of the
Crato Formation. It is housed in the URM Herbarium at the Universidade Federal de Pernam-
buco in Recife, Brazil, having been repatriated from the Illinois Natural History Survey
PLOS ONE | https://doi.org/10.1371/journal.pone.0178327 June 7, 2017 1 / 6
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OPEN ACCESS
Citation: Heads SW, Miller AN, Crane JL, Thomas
MJ, Ruffatto DM, Methven AS, et al. (2017) The
oldest fossil mushroom. PLoS ONE 12(6):
e0178327. https://doi.org/10.1371/journal.
pone.0178327
Editor: William Oki Wong, Institute of Botany,
CHINA
Received: March 26, 2017
Accepted: May 10, 2017
Published: June 7, 2017
Copyright: ©2017 Heads et al. This is an open
access article distributed under the terms of the
Creative Commons Attribution License, which
permits unrestricted use, distribution, and
reproduction in any medium, provided the original
author and source are credited.
Data Availability Statement: All relevant data are
within the paper.
Funding: This work was partly supported by US
National Science Foundation grant EF-1304622 (to
SWH) and EF-1205935 and EF-1502735 (to ANM).
Competing interests: The authors have declared
that no competing interests exist.
Paleontological Collection. It was studied using a Zeiss SteREO Discovery.V20 zoom stereomi-
croscope with a Plan-Apochromat S 0.63x f/ Reo WD = 81 mm objective. Photographs were
taken using a Canon 5D Mark III and MP-E 65 mm macro lens mounted to a Cognisys Stack-
shot motor rail on a copy stand. Multiple high-resolution images were then stacked using Heli-
conSoft’s Helicon Focus 6 and subsequently stitched together as a mosaic using Photoshop
CC. Scanning electron micrographs were produced using a JEOL JSM-6060LV SEM.
Nomenclature
The electronic version of this article in Portable Document Format (PDF) in a work with an
ISSN or ISBN will represent a published work according to the International Code of Nomen-
clature for algae, fungi, and plants, and hence the new names contained in the electronic publi-
cation of a PLOS ONE article are effectively published under that Code from the electronic
edition alone, so there is no longer any need to provide printed copies. In addition, new names
contained in this work have been submitted to MycoBank from where they will be made avail-
able to the Global Names Index. The unique MycoBank number can be resolved and the asso-
ciated information viewed through any standard web browser by appending the MycoBank
number contained in this publication to the prefix http://mycobank.org/MB/. The online ver-
sion of this work is archived and available from the following digital repositories: PubMed
Central, LOCKSS.
Results
Systematic paleontology
Kingdom Fungi (L.) Moore, 1980; Phylum Basidiomycota Moore, 1980; Class Agaricomycetes
Doweld, 2001; Order Agaricales Underwood, 1899; Family incertae sedis
Gondwanagaricites magnificus Heads, A.N. Mill. et J.L. Crane, gen. et sp. nov. (Figs 1
and 2)
[urn:lsid:mycobank.org:names:MB821206]
Holotype. Brazil: Ceara
´: Chapada do Araripe; Crato Formation: Nova Olinda Member
(Lower Cretaceous: Upper Aptian, 113–120 Ma); URM-88000. While precise locality details
are unknown, the lithology of the matrix is consistent with the specimen having been col-
lected in one of the extensive quarry complexes near the town of Nova Olinda (7.0939˚S,
39.6796˚W).
Etymology. The genus name is a combination of Gondwana, the ancient supercontinent,
the Greek word agarikon, “a mushroom,” and the Greek suffix -ites, denoting a fossil. The spe-
cific epithet is the Latin adjective magnificus, meaning “magnificent” or “splendid” in reference
to the remarkable preservation of the holotype.
Description. Basidiome color unknown (preserved as orange-brown goethitic replace-
ment). Pileus 10.0 mm diameter, 7.5 mm high at widest point; apparently circular, convex;
probably glabrous and striate; margin slightly incurved; veil absent; context 3.0 mm thick.
Lamellae (gills) 4.5 mm broad at widest point, broadly attached to stipe apex; edge entire, up to
50μm wide. Stipe 34.0 mm long, 6.5 mm wide, straight, cylindrical, with longitudinal stria-
tions, annulus absent, base slightly bulbous. Basidiospores not observed.
Comments. While Gondwanagaricites is without doubt a gilled mushroom in the Agari-
cales, familial placement is presently impossible since no evidence of basidiospores was found
during SEM examination of the specimen. The general habitus of Gondwanagaricites is remi-
niscent of mushrooms in the family Strophariaceae and placement in this family would be sup-
ported by the small size and robust shape of the overall basidiome, the thick context of the
pileus, the putative complete attachment of the gills to the central stipe, and the apparent
The oldest fossil mushroom
PLOS ONE | https://doi.org/10.1371/journal.pone.0178327 June 7, 2017 2 / 6
absence of a universal and partial veil. However, a number of other mushroom families present
similar basidiome morphology (e.g., Agaricaceae, Tricholomataceae, Bolbitiaceae, etc.) and
can only be separated by detailed studies of basidiospore shape, ornamentation, and colora-
tion. Thus, since the spores of Gondwanagaricites were not observed, we refrain from assigning
the new genus to a family.
Discussion
Fungi are ecologically diverse, geographically widespread, speciose organisms that account for
the second largest group of eukaryotes [12]. Despite their global distribution and evolutionary
history extending some 1,430 Ma [13], the fossil record for fungal structures other than spores
is exceedingly scant with reports of mostly sexual [1418] and asexual stages [1923] of asco-
mycetes from mid-Cretaceous to Miocene ambers. The Basidiomycota contains over 30,000
extant species [24], but their fossil record—especially in the case of gilled mushrooms—is
nearly non-existent due to their ephemeral nature and a strong preservational bias against
their fleshy basidiomes [18]. The earliest report of a member of the Basidiomycota is from
hyphae with diagnostic clamp connections dating c. 330 Ma from the Upper Visean (Mississip-
pian) of France [25]. Only ten fossils resembling modern-day gilled mushrooms have been
recorded to date, all from amber. The hitherto oldest fossil mushroom, Palaeoagaricites
Fig 1. Gondwanagaricites magnificus gen. et sp. nov. (A) Photomicrograph of holotype (URM 88000) showing general habitus. (B) Interpretive
drawing of (A) with major morphological features indicated. The red box indicates the position of gills shown in Fig 2.
https://doi.org/10.1371/journal.pone.0178327.g001
The oldest fossil mushroom
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antiquus, was reported from mid-Cretaceous Burmese amber (c. 99 Ma) [6]. More recently,
four unnamed mushrooms placed in the Agaricales have also been reported from Burmese
amber [8]. Archaeomarasmius leggetti was recorded from Cretaceous amber (c. 90–94 Ma)
from New Jersey, USA [3,4]. Most recently, Gerontomyces lepidotus was reported from Eocene
Baltic amber (c. 45–55 Ma) from the Samland Peninsula of Russia [7]. Three other mush-
rooms, Aureofungus yaniguaensis [5], Coprinites dominicana [2], and Protomycena electra [3,4]
have all been recorded from Early Miocene amber (Burdigalian, c. 16–18 Ma) from the
Dominican Republic.
Gondwanagaricites magnificus represents the oldest fossil record of a gilled mushroom and
is the only fossil mushroom known from a mineralized replacement. The unique specimen
extends the geological range of gilled mushrooms back by approximately 14–21 million years
and confirms their presence in Gondwana during the Early Cretaceous. Molecular clock esti-
mates suggest the divergence of the Basidiomycota around 500 Ma to 1.2 billion years [26] and
Fig 2. Scanning electron micrographs of the gills of Gondwanagaricites magnificus gen. et sp. nov.
(A) Section of preserved gills (location indicated by red box on Fig 1B). (B) close-up view of (A) showing
detailed structure.
https://doi.org/10.1371/journal.pone.0178327.g002
The oldest fossil mushroom
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G.magnificus establishes the earliest calibration point so far for the Agaricales, with a new min-
imum age of 113–120 Ma.
Acknowledgments
We thank Dra. Leonor Costa Maia of the URM Herbarium for providing a URM accession
number and for assistance repatriating the specimen to Brazil. SEM work was carried out in
the Frederick Seitz Materials Research Laboratory Central Research Facilities at the University
of Illinois. This work was partly supported by NSF grant EF-1304622 (to SWH) and EF-
1205935 and EF-1502735 (to ANM).
Author Contributions
Conceptualization: SWH.
Investigation: SWH ANM JLC MJT DMR ASM DBR.
Resources: YW.
Visualization: MJT DMR.
Writing original draft: SWH ANM JLC MJT DMR ASM.
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This beautifully illustrated 2007 volume describes the entire flora and fauna of the famous Lower Cretaceous Crato Formation of Brazil - one of the world's most important fossil deposits, exhibiting exceptional preservation. A wide range of invertebrates and vertebrates are covered, including extended sections on pterosaurs and insects. Two chapters are devoted to plants. Many of the chapters include descriptions of new species and re-descriptions and appraisals of taxa published in obscure places, rendering them available to a wider audience. Fossil descriptions are supported by detailed explanations of the geological history of the deposit and its tectonic setting. Drawing on expertise from around the world and specimens from the most important museum collections, this book forms an essential reference for researchers and enthusiasts with an interest in Mesozoic fossils.