Cho M, Neubauer P, Fahrenson C, Rechenberg I. An observational study of ballooning in large spiders: Nanoscale multifibers enable large spiders' soaring flight.
PLoS Biol 2018;
16:e2004405. [PMID:
29902191 PMCID:
PMC6001951 DOI:
10.1371/journal.pbio.2004405]
[Citation(s) in RCA: 20] [Impact Index Per Article: 2.9] [Reference Citation Analysis] [Abstract] [MESH Headings] [Track Full Text] [Download PDF] [Figures] [Journal Information] [Subscribe] [Scholar Register] [Received: 10/03/2017] [Accepted: 05/10/2018] [Indexed: 11/25/2022] Open
Abstract
The physical mechanism of aerial dispersal of spiders, “ballooning behavior,” is still unclear because of the lack of serious scientific observations and experiments. Therefore, as a first step in clarifying the phenomenon, we studied the ballooning behavior of relatively large spiders (heavier than 5 mg) in nature. Additional wind tunnel tests to identify ballooning silks were implemented in the laboratory. From our observation, it seems obvious that spiders actively evaluate the condition of the wind with their front leg (leg I) and wait for the preferable wind condition for their ballooning takeoff. In the wind tunnel tests, as-yet-unknown physical properties of ballooning fibers (length, thickness, and number of fibers) were identified. Large spiders, 16–20 mg Xysticus spp., spun 50–60 nanoscale fibers, with a diameter of 121–323 nm. The length of these threads was 3.22 ± 1.31 m (N = 22). These physical properties of ballooning fibers can explain the ballooning of large spiders with relatively light updrafts, 0.1–0.5 m s−1, which exist in a light breeze of 1.5–3.3 m s−1. Additionally, in line with previous research on turbulence in atmospheric boundary layers and from our wind measurements, it is hypothesized that spiders use the ascending air current for their aerial dispersal, the “ejection” regime, which is induced by hairpin vortices in the atmospheric boundary layer turbulence. This regime is highly correlated with lower wind speeds. This coincides well with the fact that spiders usually balloon when the wind speed is lower than 3 m s−1.
Aerial dispersal of spiders, which is known as “ballooning,” enables spiders’ wide range of dissemination—sometimes transoceanic. However, little is known about the ballooning mechanism of spiders, due to the difficulty of observing the ballooning silks and little awareness of spiders’ ballooning flight itself. From our observations in the field and in the laboratory using a wind tunnel, we have characterized the heretofore unknown physical properties of spiders’ ballooning silks. These quantitative values can explain large spiders’ ballooning behaviors. Crab spiders use tens of nanoscale fibers for their aerial dispersal. In the air current, these nanoscale fibers are governed by low Reynolds number fluid dynamics, which means that the viscous force of the air is much more dominant than the inertial force of the air. Using this nano/microscale fluid dynamics, spiders can become airborne with a light updraft. From our wind measurements, we suggest that spiders use the organized updraft current in the turbulent wind. This may explain why spiders show the ballooning behavior at a low wind speed, as the updraft frequently exists in the low-speed regime of the fluctuating wind flows. This work represents the most rigorous investigation of spider ballooning to date and will inspire future research on the subject.
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