量化密苏里州中北部高草大草原残存区和恢复区的种子雨模式

bioRxiv Pub Date : 2024-07-16 DOI:10.1101/2024.07.10.602969
K. C. Wynne, M. J. Parker-Smith, Erica M. Murdock, Lauren L. Sullivan
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摘要

种子雨是一个与植物群落多样性、组成和再生有关的影响过程。然而,对种子雨模式的了解仅限于在森林和晚期集结的草地上观察到的模式,这可能无法反映新恢复草地等早期集结群落的情况。解决这一认识上的空白,有助于我们进一步了解种子传播的作用。在这里,我们测量了一个残存高草草原的种子雨,该草原是1978年草原种子雨基础研究的地点,也是附近高草草原恢复的时间序列。我们试图确定种子雨的数量、种子质量特征、时间、多样性和组成在(1)长期和(2)群落集结期间发生了怎样的变化。为此,我们在 2 年、5-6 年和 15 年的恢复草原和残留草原上部署了人工草皮草籽诱捕器,从 2019 年 5 月到 12 月,每两周更换一次诱捕器。与 1978 年相比,2019 年我们在残存草原捕获的种子雨密度和丰富度增加了一倍多。我们还发现,随着草原年龄的增长,种子雨模式也发生了变化,每片草原都拥有独特的散播物种群落。在最年轻的恢复草原上,捕获到的种子、种子生物量和物种明显更多。不过,所有草原的种子质量特征都很相似。除了成分外,最老的恢复草原的所有其他种子雨指标最终都与残存草原相当。综述与应用:我们的研究结果表明,草原,尤其是年轻的草原,产生的种子雨量(124,806 粒种子 m-2 年-1,97.24 g m-2 年-1)比之前已知的要大,所有取样草原的种子输入量都远远超过了恢复后的播种密度。我们还发现,整个时序中种子雨量的减少与种子质量的增加并不一致,这表明这些指标之间缺乏权衡。此外,高草草原的恢复并没有复制残存系统中的种子雨成分。可能需要提高理想物种的恢复播种率以达到组成目标,因为目前的播种率可能无法与新恢复草原中发现的不良物种的繁殖压力相抗衡。
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Quantifying seed rain patterns in a remnant and a chronosequence of restored tallgrass prairies in north central Missouri
Seed rain is an influential process related to plant community diversity, composition, and regeneration. However, knowledge of seed rain patterns is limited to those observed in forests and late-assembling grasslands, which might not reflect early-assembling communities such as newly restored grasslands. Resolving this gap in our understanding provides further insight into the role of seed dispersal. Here, we measured seed rain in a remnant tallgrass prairie, which was the site of the foundational grassland seed rain study in 1978, and a nearby chronosequence of tallgrass prairie restorations. We sought to determine how the quantity, seed mass traits, timing, diversity, and composition of seed rain changed (1) long-term and (2) during community assembly. To do so, we deployed artificial turf grass seed traps into 2-year-old, 5-6-year-old, and 15-year-old restored prairies and the remnant prairie, replacing traps every two weeks from May to December 2019. We captured over twice the density and richness of seed rain in the remnant prairie in 2019 compared to 1978. We also found that seed rain patterns changed as prairies aged, with each prairie possessing a distinct community of dispersing species. Significantly more seeds, seed biomass, and species were captured in the youngest restored prairie. However, seed mass traits were similar in all prairies. Except for composition, all other seed rain metrics in the oldest restoration were eventually comparable to the remnant prairie. Synthesis and Applications: Our results revealed that grasslands, notably young prairies, produce larger quantities of seed rain than previously known (124,806 seeds m−2 year −1, 97.24 g m−2 year −1), and seed input in all sampled prairies far exceeded restoration broadcast seeding densities. We further found that decreases in seed rain quantity across the chronosequence did not correspond with increases in seed mass, suggesting a lack of tradeoffs between these metrics. Furthermore, tallgrass prairie restorations have not replicated the composition of seed rain seen in remnant systems. Increasing restoration seeding rates of desirable species may be needed to meet composition goals since current rates may not compete with the propagule pressure of undesirable species found in newly restored prairies.
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