Effects of grazing on grassland soil carbon: a global review

Soils of grasslands represent a large potential reservoir for storing CO₂, but this potential likely depends on how grasslands are managed for large mammal grazing. Previous studies found both strong positive and negative grazing effects on soil organic carbon (SOC) but explanations for this variation are poorly developed. Expanding on previous reviews, we performed a multifactorial meta‐analysis of grazer effects on SOC density on 47 independent experimental contrasts from 17 studies. We explicitly tested hypotheses that grazer effects would shift from negative to positive with decreasing precipitation, increasing fineness of soil texture, transition from dominant grass species with C₃ to C₄ photosynthesis, and decreasing grazing intensity, after controlling for study duration and sampling depth. The six variables of soil texture, precipitation, grass type, grazing intensity, study duration, and sampling depth explained 85% of a large variation (±150 g m^?2 yr^?1) in grazing effects, and the best model included significant interactions between precipitation and soil texture (P = 0.002), grass type, and grazing intensity (P = 0.012), and study duration and soil sampling depth (P = 0.020). Specifically, an increase in mean annual precipitation of 600 mm resulted in a 24% decrease in grazer effect size on finer textured soils, while on sandy soils the same increase in precipitation produced a 22% increase in grazer effect on SOC. Increasing grazing intensity increased SOC by 6–7% on C₄‐dominated and C₄–C₃ mixed grasslands, but decreased SOC by an average 18% in C₃‐dominated grasslands. We discovered these patterns despite a lack of studies in natural, wildlife‐dominated ecosystems, and tropical grasslands. Our results, which suggest a future focus on why C₃ vs. C₄‐dominated grasslands differ so strongly in their response of SOC to grazing, show that grazer effects on SOC are highly context‐specific and imply that grazers in different regions might be managed differently to help mitigate greenhouse gas emissions.     

Impact of climatic variation on populations of pine processionary moth Thaumetopoea pityocampa in a core area of its distribution

• 1 There is growing appreciation of climatic effects on insect population dynamics at the margins of distribution limits. Climatic effects might be less important and/or involve different drivers and processes near the centre of distributions.
• 2 We evaluated the effects of interannual variation in temperatures, radiation and precipitation on populations of pine processionary moth Thaumetopoea pityocampa in Central–South Portugal, a low altitude area with a relatively mild Mediterranean climate near the centre of the north–south range of the species.
• 3 We tested for effects of climate on mortality of young larvae, growth rates, final larval mass and fecundity.
• 4 Results indicated high mortality of early instars associated with low minimum and maximum daily temperatures and low precipitation. Low minimum temperatures were further associated with high parasitism by the larval parasitoid Phryxe caudata (Rondani) (Diptera, Tachinidae). Furthermore, larval growth rates were higher with high solar radiation during December and January, which was itself negatively related to precipitation and air temperature. Slow larval growth rates led to lower final mass at pupation in the spring, and smaller egg masses and smaller initial colony sizes during the next autumn.
• 5 Thus climatic factors, and temperature in particular, apparently contributed to population dynamics of T. pityocampa in the core of its distribution, as well as at its northern limits. The most specific climatic parameters of importance, however, and the connections between climate, physiology and insect demographics in the core area were clearly different from northern areas.

     

The Influences of Environment, Mating Habitat, and Predation on Evolution of Pinniped Lactation Strategies

Seals have adapted their social systems and lactation strategies to marine environments that include open and ice-covered oceans, high and low productivity, extremes in seasonality, and ocean- and terrestrial-type predators. Different explanations for the variation in pinniped lactation systems have been proposed but tests of alternative hypotheses have not sufficiently accounted for phylogeny and body size. After controlling for this variation, I predicted that environment, mating habitat, and predation would yield a fuller explanation. Lactation traits, duration, pup growth rate, and fat content were significantly influenced by both body size and phylogeny, which together explained 20–69% of the variation. After controlling for this variation, initial results did not support the environment hypothesis, as no differences in lactation traits were found between species living in polar (≥60°N) versus equatorial (<60°N) environments. In contrast, seals that nurse in areas of Arctic sea ice contending with ice-hunting predators, such as polar bears, had relatively short lactation compared to species living in the Antarctic and more equatorial regions. Also, the availability of predator-free islands for terrestrial mating and parturition was related to a harem mating system, increased sexual size dimorphism (SSD), and slow juvenile growth rates, less fat in milk, and longer lactation. Using structural equation modeling, latitude and size of harems provided independent explanations for all three lactation traits. Thus, use of islands in ice-free waters, predation in Arctic ice-covered waters, and more milk fat in high-latitude seals together provided adequate explanations for the evolution of lactation diversity among pinnipeds.     

施入不同土层的秸秆腐殖化特征及对玉米产量的影响

耕作和秸秆还田是打破犁底层、改善黑土肥力的重要措施.本研究利用田间试验,分析了耕作和秸秆还田对秸秆腐殖化系数、总有机质含量(SOC)和玉米产量的影响.结果表明:深耕+秸秆施入20～35 cm(ST+S)能够打破犁底层,与浅耕(TT)、深耕(ST)和浅耕+秸秆还田(TT+S)相比,试验6年间土壤容重平均降低了5.7%、3.3%和5.7%,其中ST和ST+S试验第一年效果最好;试验6年后秸秆腐解率表现为0～20 cm土层(72.0%)>20～35 cm土层(59.2%);0～20和20～35 cm土层秸秆腐殖化系数在试验的第一年达到了最大值,分别为15.9%和12.7%;与初始土壤相比,TT、ST和ST+S处理0～20 cm土层SOC和轻组有机碳(LFOC)含量呈下降趋势,而TT+S处理分别增加了2.9%和12.4%,ST+S处理20～35 cm土层分别增加了9.2%和9.9%;对玉米产量的影响表现为ST+S>TT+S>ST>TT,耕作和秸秆还田的时间效应明显,其中ST处理玉米产量的影响可以持续3年,而ST+S处理可以持续6年.因此,通过耕作的方式将秸秆施入20～35 cm土层是一种有效的、可持续改善黑土质量的农业措施.     

中华羊茅内生真菌Neotyphodium sp.生物学与生理学特性的研究

本文对中华羊茅Festuca sinensis内生真菌Neotyphodium sp.的生物学与生理学特性进行了报道。研究发现:中华羊茅内生真菌能在10-30℃生长,5℃和35℃几乎不能生长,最适生长温度是25℃;适宜的pH是7-9;不同的碳、氮源利用能力不同,利用能力最好的分别是甘露醇和酵母浸液;在不同培养基上的生长速度与产孢特性存在差异,马铃薯葡萄糖琼脂(PDA)培养基上生长最快,水琼脂(WA)和海水营养琼脂(SNA)培养基上生长最慢,但WA和SNA产孢最多。     

布氏田鼠种群繁殖特征研究

越冬田鼠每年可繁殖3胎,第1胎幼仔生于4月下旬到6月上旬,第2胎幼仔生于5月中旬到7月上旬,第3胎幼仔生于6月中旬到7月下旬。种群上升年份(1987)各胎幼仔出生高峰比1988年的提前10天左右。1987年越冬鼠第1胎集中,如4月下半月,1987年怀孕率为100%,而1988年只有44.44%。6月上半月以前越冬鼠为种群繁殖的主体,而后被当年生鼠所取代。从4月下半月到9月上半月共出生4批同龄群。K₁和K₂组生长发育旺盛,当年就参加种群繁殖,可怀孕1—3胎。K₃组生长发育较慢,当年并不性成熟,越冬后性成熟成为种群越冬鼠的主体。K₄出生晚,数量少,很少能度过漫长寒冷的冬季而成为种群的无用或潜在的繁殖力量。本文还发现越冬鼠的平均胎仔数显著高于当年鼠：种群上升年份越冬鼠平均胎仔数高于种群下降年份,而当年生鼠的平均胎仔数年度间则没有显著性差异。