Abstract
Despite the well-recognized importance of plant traits for biogeomorphic development of landscapes, our understanding remains limited of how species-specific plant traits respond to and serve as drivers for the sedimentary dynamics within a biogeomorphic landscape. By manipulating a series of laboratory experiments, using mesocosms and a flume, we examined how species-specific differences in expansion strategy, i.e., clonal step-length of laterally expanding tillers, both respond to sediment type and drive cliff formation and persistence. We compared three marsh species, with contrasting clonal expansion traits, that are dominant in many estuaries worldwide: Spartina anglica, Scirpus maritimus, and Phragmites australis. Our results revealed that S. anglica tussocks tend to have high shoot density due to a short clonal expansion step-length, whereas S. maritimus tussocks were much more diffuse and tend to have a longer clonal expansion step-length. P. australis showed intermediate traits. Clonal expansion step-length did show within-species variation in response to sediment texture, but species-specific differences remained the most important. Species with smaller clonal step-lengths, such as S. anglica in this study, are more likely to induce cliffs at the marsh edge by driving formation of larger cliff heights and also having lower capacity to grow out from cliffs. Our findings thus illustrate how dynamic landscape features like cliffs at marsh edges depend on the clonal expansion traits of the dominant species. This enhances current understanding of the formation and development of marsh edges, and is instructive for understanding the role of species-specific traits in driving distinct biogeomorphic landscape dynamics.
Original language | English |
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Pages (from-to) | 3754-3767 |
Number of pages | 14 |
Journal | Limnology and Oceanography |
Volume | 66 |
Issue number | 10 |
DOIs | |
Publication status | Published - Oct 2021 |
Bibliographical note
Funding Information:We thank Daniel Blok, Lennart van IJzerloo, Jeroen van Dalen, and Bert Sinke from NMF of the NIOZ, for their kind help setting up the experiment. This work was supported by the project “Coping with deltas in transition” within the Programme of Strategic Scientific Alliances between China and the Netherlands (PSA), financed by the Chinese Ministry of Science and Technology (MOST), Project no. 2016YFE0133700; the Royal Netherlands Academy of Arts and Sciences (KNAW), Project no. PSA‐SA‐E‐02; the National Natural Science Foundation of China (Grant No: 41876093); and the CoE‐Rammegors project of the Netherlands. Z. Z. is. supported by the Program for Guangdong Introducing Innovative and Entrepreneurial Teams (2019ZT08L213).
Funding Information:
We thank Daniel Blok, Lennart van IJzerloo, Jeroen van Dalen, and Bert Sinke from NMF of the NIOZ, for their kind help setting up the experiment. This work was supported by the project ?Coping with deltas in transition? within the Programme of Strategic Scientific Alliances between China and the Netherlands (PSA), financed by the Chinese Ministry of Science and Technology (MOST), Project no. 2016YFE0133700; the Royal Netherlands Academy of Arts and Sciences (KNAW), Project no. PSA-SA-E-02; the National Natural Science Foundation of China (Grant No: 41876093); and the CoE-Rammegors project of the Netherlands. Z. Z. is. supported by the Program for Guangdong Introducing Innovative and Entrepreneurial Teams (2019ZT08L213).
Publisher Copyright:
© 2021 The Authors. Limnology and Oceanography published by Wiley Periodicals LLC on behalf of Association for the Sciences of Limnology and Oceanography.
Funding
We thank Daniel Blok, Lennart van IJzerloo, Jeroen van Dalen, and Bert Sinke from NMF of the NIOZ, for their kind help setting up the experiment. This work was supported by the project “Coping with deltas in transition” within the Programme of Strategic Scientific Alliances between China and the Netherlands (PSA), financed by the Chinese Ministry of Science and Technology (MOST), Project no. 2016YFE0133700; the Royal Netherlands Academy of Arts and Sciences (KNAW), Project no. PSA‐SA‐E‐02; the National Natural Science Foundation of China (Grant No: 41876093); and the CoE‐Rammegors project of the Netherlands. Z. Z. is. supported by the Program for Guangdong Introducing Innovative and Entrepreneurial Teams (2019ZT08L213). We thank Daniel Blok, Lennart van IJzerloo, Jeroen van Dalen, and Bert Sinke from NMF of the NIOZ, for their kind help setting up the experiment. This work was supported by the project ?Coping with deltas in transition? within the Programme of Strategic Scientific Alliances between China and the Netherlands (PSA), financed by the Chinese Ministry of Science and Technology (MOST), Project no. 2016YFE0133700; the Royal Netherlands Academy of Arts and Sciences (KNAW), Project no. PSA-SA-E-02; the National Natural Science Foundation of China (Grant No: 41876093); and the CoE-Rammegors project of the Netherlands. Z. Z. is. supported by the Program for Guangdong Introducing Innovative and Entrepreneurial Teams (2019ZT08L213).