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21.
'15N signatures of fossil peat were used to interpret past ecosystem processes on tectonically active subantarctic Macquarie Island. By comparing past vegetation reconstructed from the fossil record with present-day vegetation analogues, our evidence strongly suggests that changes in the '15N signatures of fossil peat at this location reflect mainly past changes in the proportion of plant nitrogen derived from animal sources. Associated with uplift above sea level over the past 8,500 years, fossil records in two peat deposits on the island chronicle a change from coastal vegetation with fur and elephant seal disturbance to the existing inland herbfield. Coupled with this change are synchronous changes in the '15N signatures of peat layers. At two sites 15N-enriched peat '15N signatures of up to +17‰ were associated with a high abundance of pollen of the nitrophile Callitriche antarctica (Callitrichaceae). At one site fossil seal hair was also associated with enriched peat '15N. Less 15N enriched '15N signatures (e.g. -1.9‰ to +3.9‰) were measured in peat layers which lacked animal associated C. antarctica and Acaena spp. Interpretation of a third peat profile indicates continual occupation of a ridge site by burrowing petrels for most of the Holocene. We suggest that 15N signatures of fossil peat remained relatively stable with time once deposited, providing a significant new tool for interpreting the palaeoecology.  相似文献   
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  1. Plant–animal interactions are diverse and widespread shaping ecology, evolution, and biodiversity of most ecological communities. Carnivorous plants are unusual in that they can be simultaneously engaged with animals in multiple mutualistic and antagonistic interactions including reversed plant–animal interactions where they are the predator. Competition with animals is a potential antagonistic plant–animal interaction unique to carnivorous plants when they and animal predators consume the same prey.
  2. The goal of this field study was to test the hypothesis that under natural conditions, sundews and spiders are predators consuming the same prey thus creating an environment where interkingdom competition can occur.
  3. Over 12 months, we collected data on 15 dates in the only protected Highland Rim Wet Meadow Ecosystem in Kentucky where sundews, sheet‐web spiders, and ground‐running spiders co‐exist. One each sampling day, we attempted to locate fifteen sites with: (a) both sheet‐web spiders and sundews; (b) sundews only; and (c) where neither occurred. Sticky traps were set at each of these sites to determine prey (springtails) activity–density. Ground‐running spiders were collected on sampling days. DNA extraction was performed on all spiders to determine which individuals had eaten springtails and comparing this to the density of sundews where the spiders were captured.
  4. Sundews and spiders consumed springtails. Springtail activity–densities were lower, the higher the density of sundews. Both sheet‐web and ground‐running spiders were found less often where sundew densities were high. Sheet‐web size was smaller where sundew densities were high.
  5. The results of this study suggest that asymmetrical exploitative competition occurs between sundews and spiders. Sundews appear to have a greater negative impact on spiders, where spiders probably have little impact on sundews. In this example of interkingdom competition where the asymmetry should be most extreme, amensalism where one competitor experiences no cost of interaction may be occurring.
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Abstract .The effect of the introduction of the entomophagous copepod Mesocyclops longisetus (Acuacultura F.C.B. strain) on the survival of Aedes aegypti immature stages in car tyres was evaluated under semi-natural conditions in the municipality of Merida, Yucatan, Mexico. Life tables were constructed for the immature stages of the mosquito in the presence and absence of M. longisetus , and the survival data were compared using log–linear models. The data set was adjusted using the GLIM statistical package and the quality of adjustment was evaluated with a chi-squared test . Survivorship curves were constructed for each treatment.
In the absence of M. longisetus , the survivorship of Ae. aegypti immature stages averaged 9%. The highest mortality rate was observed during the fourth larval instar (54%) and the resulting survival pattern corresponded to a type II survivorship curve. The mortality rate of Ae. aegypti first-instar larvae (fifty per tyre) increased more than 200-fold in the presence of M. longisetus (twenty per tyre) and the highest mortality was during the first two larval instars, where it reached 98.9%, with a resulting survivorship of 0.2%. Overall mortality was sixfold greater in the presence of the copepod than in its absence. The survival pattern of immature stages of Ae. aegypti in the presence of the copepod corresponded to a type III survivorship curve. As M. longisetus was so effective against Ae. aegypti immature stages in tyres under semi-natural conditions, its long-term effectiveness should be evaluated under socially and ecologically realistic field conditions in Mexico.  相似文献   
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Zoosporic true fungi are thought to be ubiquitous in many ecosystems, especially in cool, moist soils and freshwater habitats which are rich in organic matter. However, some of the habitats where these fungi are found may periodically experience extreme conditions, such as soils in extremely dry, hot and cold climates, acidic and alkaline soils, polluted rivers, anaerobic soil and water, saline soil and water, periglacial soils, oligotrophic soils, tree canopies and hydrothermal vents. It is clear that many ecotypes of zoosporic true fungi have indeed adapted to extreme or stressful environmental conditions. This conclusion is supported by studies in both the field and in the laboratory. Therefore, in our opinion, at least some true zoosporic fungi can be considered to be extremophiles.  相似文献   
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Zusammenfassung Der kohlensaure Kalk der untersuchten Helicideneischalen — Bulimus maximus (Durchmesser der Schale 23,6 x 25,1 mm, Dicke 0,25 mm), nicht näher bestimmte Schneckeneischale aus Sta. Catharina Brazil (Durchmesser 22,5 x 16,3 mm, Dicke 0,15 mm) — ist Calcit gemäß Optik (negativ einachsiges Konoskopbild) and Meigenscher Reaktion (in Übereinstimmung mit Kellys Beobachtungen bei Bulimus oblongus). Der Phosphatgehalt der Schale ist äuBerst gering trotz reichlichen Vorkommens der KELLyschen Phosphatkörnehen; diese sind in Wirklichkeit Gaseinschüisse. Erhitzen von Schalenstiicken braunt den Kalk bei Verkohlung der organischen Substanz durch and durch ; these durchsetzt also die Calcitkristalle, in Übereinstimmung mit Kellys Erfahrungen beim Entkalken. Erhitzen his zum Verbrennen der organischen Substanz (Wiederweißwerden der Schalenstücke) hebt die Doppelbrechung auf (Umwandlung des Calciumcarbonats in -oxyd); zugleich erscheint bräunliche Trübung im durchfallenden Licht wohl infolge des Austretens der Kohlensäure.Die Mammillenschicht auf der Innenseite der Schale besteht aus einzelnen Calcitindividuen oder Gruppen von solchen; diese Kristallkörnchen wachsen (zum Teil) zu den annähernd senkrecht stehenden Prismen aus, deren optische Achse rneist gegen die Schalenfläche geneigt ist. Vor allem bei Bulimus maximus lassen die Prismen eine innere grobgeschichtete and eine äußere feinstreifige Lage unterscheiden; die erste enthält die Gaseinschliisse, die sich bei der Schneckeneischale aus Sta. Catharina Brazil bis in die Mammillen hinein finden, and von rundlicher Form sind, während she bei Bulimus maximus zum Teil spaltenartig erscheinen. An manchen Stellen der Eischale aus Sta. Catharina Brazil tragen die Mamillen an ihrem freien Ende Scheiben aus radial gestellten Kalknadeln oder Rosetten aus größeren Kristallen, die bis zur Berührung benachbarter auswachsen können.  相似文献   
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