Abstract
Effective seed dispersal is critical for enabling rapid state shift from a bare tidal flat to a vegetated marsh. While tidal currents are the main dispersal vector in coastal environments, biological characteristics that keep seeds afloat have been shown to influence primary seed dispersal, i.e., seed departure from the parent plant. In contrast, secondary seed dispersal processes that move (germinated) seeds trapped within microsites have been largely neglected. Here, we explore the extent to which the coupling between biotic traits and abiotic factors affects secondary seed dispersal, and whether secondary seed dispersal may explain sudden saltmarsh establishment (i.e., rapid colonization of bare tidal flat by large numbers of seedlings in spring). We used two widely spread pioneer species: Scripus mariqueter and Spartina alterniflora. Combined flume and field results demonstrated that: (1) germination stage, current velocity, and sedimentary regime have a marked effect on the probability of secondary seed dispersal by influencing the threshold lift-off velocity of (germinated) seeds within microsites; (2) density and bud length are critical biotic traits that best predict the potential of secondary-dispersal onset after seed germination; (3) S. alterniflora possess a stronger secondary dispersal ability compared to S. mariqueter; and (4) secondary dispersal of germinated seeds in spring may explain observed sudden marsh establishment on bare tidal flats. Our findings provide novel insight relevant to understanding the drivers of seed dispersal and thereby sudden saltmarsh establishment events, with important implications for understanding the effects of climate change on critical state transitions and enabling human-aided restoration.
| Original language | English |
|---|---|
| Pages (from-to) | 3070-3084 |
| Number of pages | 15 |
| Journal | Limnology and Oceanography |
| Volume | 66 |
| Issue number | 8 |
| DOIs | |
| Publication status | Published - Aug 2021 |
Bibliographical note
Funding Information:The authors would like to acknowledge the Chongming Dongtan Nature Reserve and Yangtze Delta Estuarine Wetland Ecosystem Observation and Research Station for providing the necessary support when conducting this study. We give our heartfelt thanks to Jianwei Sun, Jinlei Zhang, Jialin Pan, Xianye Wang, and Yang Li for their help preparing and establishing the flume experiments. Special thanks are given to Haobing Cao and Jim van Belzen for their constructive comments on an earlier version of the manuscript. T.J.B. acknowledges the RWS‐funded Perkpolder project and the Zuidgors project, which was funded by the Province of Zeeland; both aim to obtain a better understanding of salt‐marsh establishment. .L.Y. and L.Z. were supported by the National Natural Science Foundation of China (41876093) and the National Key R&D Program of China (2016YFE0133700). Z.Z. also acknowledges financial support from the China Scholarship Council.
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
The authors would like to acknowledge the Chongming Dongtan Nature Reserve and Yangtze Delta Estuarine Wetland Ecosystem Observation and Research Station for providing the necessary support when conducting this study. We give our heartfelt thanks to Jianwei Sun, Jinlei Zhang, Jialin Pan, Xianye Wang, and Yang Li for their help preparing and establishing the flume experiments. Special thanks are given to Haobing Cao and Jim van Belzen for their constructive comments on an earlier version of the manuscript. T.J.B. acknowledges the RWS‐funded Perkpolder project and the Zuidgors project, which was funded by the Province of Zeeland; both aim to obtain a better understanding of salt‐marsh establishment. .L.Y. and L.Z. were supported by the National Natural Science Foundation of China (41876093) and the National Key R&D Program of China (2016YFE0133700). Z.Z. also acknowledges financial support from the China Scholarship Council.
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
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