Human disturbance affects the long-term spatial synchrony of freshwater invertebrate communities

2015 ◽  
Vol 196 ◽  
pp. 300-308 ◽  
Author(s):  
M.J. Feio ◽  
S. Dolédec ◽  
M.A.S. Graça
2015 ◽  
Vol 282 (1806) ◽  
pp. 20150173 ◽  
Author(s):  
Ayco J. M. Tack ◽  
Tommi Mononen ◽  
Ilkka Hanski

Climate change is known to shift species' geographical ranges, phenologies and abundances, but less is known about other population dynamic consequences. Here, we analyse spatio-temporal dynamics of the Glanville fritillary butterfly ( Melitaea cinxia ) in a network of 4000 dry meadows during 21 years. The results demonstrate two strong, related patterns: the amplitude of year-to-year fluctuations in the size of the metapopulation as a whole has increased, though there is no long-term trend in average abundance; and there is a highly significant increase in the level of spatial synchrony in population dynamics. The increased synchrony cannot be explained by increasing within-year spatial correlation in precipitation, the key environmental driver of population change, or in per capita growth rate. On the other hand, the frequency of drought during a critical life-history stage (early larval instars) has increased over the years, which is sufficient to explain the increasing amplitude and the expanding spatial synchrony in metapopulation dynamics. Increased spatial synchrony has the general effect of reducing long-term metapopulation viability even if there is no change in average metapopulation size. This study demonstrates how temporal changes in weather conditions can lead to striking changes in spatio-temporal population dynamics.


2011 ◽  
Vol 184 (11) ◽  
pp. 6923-6934 ◽  
Author(s):  
Astrid V. Stronen ◽  
Nathan H. Schumaker ◽  
Graham J. Forbes ◽  
Paul C. Paquet ◽  
Ryan K. Brook

2006 ◽  
Vol 42 ◽  
pp. S150-S156 ◽  
Author(s):  
M.A. Callaham ◽  
D.D. Richter ◽  
D.C. Coleman ◽  
M. Hofmockel

2015 ◽  
Vol 35 (1) ◽  
pp. 218-232 ◽  
Author(s):  
Simone Hasenbein ◽  
Sharon P. Lawler ◽  
Juergen Geist ◽  
Richard E. Connon

Author(s):  
I. D. M. Gunn ◽  
M. T. O’Hare ◽  
P. S. Maitland ◽  
L. May

Hydrobiologia ◽  
2020 ◽  
Vol 847 (18) ◽  
pp. 3711-3725 ◽  
Author(s):  
Yintao Jia ◽  
Mark J. Kennard ◽  
Yuhan Liu ◽  
Xiaoyun Sui ◽  
Kemao Li ◽  
...  

Hydrobiologia ◽  
2011 ◽  
Vol 681 (1) ◽  
pp. 59-72 ◽  
Author(s):  
I. D. M. Gunn ◽  
M. T. O’Hare ◽  
P. S. Maitland ◽  
L. May

Diversity ◽  
2021 ◽  
Vol 13 (11) ◽  
pp. 599
Author(s):  
Manuela Abelho ◽  
Rui Ribeiro ◽  
Matilde Moreira-Santos

We evaluated the effect of seawater intrusion in coastal ecosystems on the freshwater invertebrate community and on leaf litter decomposition under realistic scenarios in six outdoor freshwater mesocosms containing fauna and flora, to which increasing volumes of seawater were added. The resulting salinity values were 0.28 (control, freshwater only), 2.0, 3.3, 5.5, 9.3, and 15.3 mS cm−1. The effect of salinity was assessed for 65 days after seawater intrusion, by computing the deviation of values in each treatment in relation to the control. Our results show that seawater intrusion into freshwaters will affect the invertebrate communities and organic matter decomposition, with salinities of up to 3.3–5.5 mS cm−1 having opposite effects to salinities of more than 9.3 mS cm−1. There was a net negative effect of the two highest salinities on mass loss and richness of the invertebrates associated with the decomposing leaves. Regarding the invertebrate communities of the mesocosms, there was a net negative effect of the intermediate salinity levels on abundance and richness. Invertebrate life cycle traits conferring resilience and resistance tended to increase with low and decrease with high salinity values, while avoidance traits showed an opposite trend, and these responses were more pronounced on the later stage community. These wave-like responses of the invertebrate species traits to increasing salinity suggest that the life-history and physiological adaptations most suitable to cope with osmotic stress will differ between low and high salinity levels.


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