Nurse logs: A common seedling strategy in the Permian Cathaysian floraShow others and affiliations
2022 (English)In: iScience, E-ISSN 2589-0042 , ISSN 2589-0042, Vol. 25, p. 1-11, article id 105433Article in journal (Refereed) Published
Abstract [en]
Nurse logs are common in modern forests from boreal to temperate and tropical ecosystems. However, the evolution of the nurse-log strategy remains elusive because of their rare occurrence in the fossil record. We report seven coniferous nurse logs from lowermost to uppermost Permian strata of northern China that have been colonized by conifer and sphenophyllalean roots. These roots are associated with two types of arthropod coprolites and fungal remains. Our study provides the first glimpse into plant—plant facilitative relationships between late Paleozoic gymnosperms and sphenopsids. Detritivorous arthropods and fungi appear to have been crucial for the utilization of nurse logs in Permian forests. The phylogenetically distant roots demonstrate that nurse-log interaction wasa sophisticated seedling strategy in late Paleozoic humid tropical forests, and this approach may have been adopted and developed by a succession of plant groups leading to its wide representation in modern forest ecosystems.
Place, publisher, year, edition, pages
Cambridge, Massachusetts, 2022. Vol. 25, p. 1-11, article id 105433
Keywords [en]
plant regeneration, Permian, Gigantopteridales, nurse logs, seedlings, fungi, coprolites
National Category
Other Earth and Related Environmental Sciences
Research subject
The changing Earth
Identifiers
URN: urn:nbn:se:nrm:diva-4887DOI: 10.1016/ j.isci.2022.105433OAI: oai:DiVA.org:nrm-4887DiVA, id: diva2:1714931
Funder
Swedish Research Council, 2018-04527
Note
This study was supported jointly by the Strategic Priority Research Program of Chinese Academy of Sciences (XDB26000000), the Second Tibetan Plateau Scientific Expedition and Research (2019QZKK0706), the Yunnan Provincial Science and Technology Department (2019FJ010), and the Key Research Program of the Institute of Geology and Geophysics, Chinese Academy of Sciences (IGGCAS-201905). S.M. is funded by a grant from the Swedish Research Council (VR grant number 2018-04527).
2022-11-302022-11-30Bibliographically approved