Orientation of crustacean burrows

Most arthropod burrows show a marked preferred orientation: they are not random in alignment. A recent burrow made by Jaxea nocturna Nardo is compared to three fossil burrows from the Austrian Tertiary. In each system very steep and very flat burrow sections can be distinguished. In three cases, including the Recent one, flat burrow sections dominate in length. In all burrow sections the distribution of trend angles is also not uniform but indicate preferred directions. In those cases where two mean vectors exist their position is nearly orthogonal, in systems with three mean vectors they form angles of nearly 60°. A relationship between these preferred directions to coastline orientation and current direction is likely.     

Lobster burrows in Swedish waters

Summary 1. The typical habitat of the European lobster(Homarus vulgaris) is rocky or soft bottom with crevices, boulders and stones.2. At the Swedish west coast it favours a bottom with stones and boulders on sand or shellsand, where it can dig burrows in the soft bottom material under the stones or boulders.3. Such burrows have one, or more than one, opening; in the latter case usually two. A relationship between the size of a lobster and its burrow is often, but not always, noted. The lengths of tunnel-formed burrows, for instance, vary with the size of the overlying stones.4. External factors more or less important in the choice of the site of a burrow are, for example, the composition of the bottom material, the occurrence of slightly overhanging edges of stones or rocks, an outwards-downwards sloping bottom, highest possible values of salinity and temperature, and a sparse algal vegetation or no vegetation at all. Lobsters tend to be absent from polluted areas where the sedimentation rate of organic particles and the turbidity of the water are high.5. Besides being shelters, the burrows also serve as look-outs.6. Burrows may be dug in soft-bottom material in rocky crevices or in flat mud bottoms.7. The burrowing behaviour is characterized by three main patterns: (a) loosening of the bottom material with the walking legs and sometimes with the big claws, (b) shuffling off of piles of soft bottom material in a basket formed by the 3rd pair of maxillipeds and one or two pairs of walking legs, and (c) fanning backwards with the pleopods.8. Small lobsters behave like adults.9. The burrowing behaviour is very similar to that of the American lobster and resembles that ofNephrops norvegicus.

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Hummerhöhlen in schwedischen Gewässern

Kurzfassung Der europäische Hummer(Homarus vulgaris) wird vorzugsweise auf felsigen Böden mit Löchern und Spalten und felsigen oder sandigen Böden mit Steinblöcken und kleineren Steinen angetroffen. Vereinzelte Individuen sieht man auch auf ebenen Weichböden. Besonders tagsüber weilen die Tiere gern in Löchern bzw. Höhlen, welche die Hummer unter Steinen, Blöcken oder an Felswänden selbst ausgegraben haben. Viele Faktoren wirken bei der Wahl des Standortes zusammen, an dem eine solche Höhle ausgegraben werden soll. Unter Steinen und Felsen — vorzugsweise mit überhängenden Kanten — muß geeignetes Bodenmaterial vorhanden sein. Günstige hydrographische Verhältnisse sind eine weitere Voraussetzung. Fernerhin muß der Boden außerhalb der Höhle etwas schräggelagert sein; die Algenvegetation darf nicht zu dicht sein, damit die Sicht nicht eingeschränkt wird. Eine von einem anderen Hummer oder von einem Taschenkrebs verlassene Höhle nimmt der Hummer gerne in Besitz und verbessert sie, falls es notwendig ist. Verschmutzte Gewässer mit erheblicher Sedimentation und starker Trübung werden nicht besiedelt. Die meisten der gegrabenen Hummerhöhlen haben eine Öffnung. Einige sind in der Art eines Tunnels gebaut, mit zwei — selten drei — Öffnungen. Eine gewisse Relation zwischen der Größe einer Höhle und der des einwohnenden Hummers ist vorhanden. Oft aber bestimmt das Aussehen der unmittelbaren Umgebung die Größe der Höhle: so ist die Dimension eines oben liegenden Steines entscheidend für die Länge eines Tunnels. Auch in Lehmböden findet man ausnahmsweise gegrabene Höhlen. Die Art und Weise, in der der Hummer seine Höhle gräbt, wird kurz beschrieben. Die Arbeitsweise ist im Grunde stereotyp, sie wird aber zum Teil den speziellen Verhältnissen der Umgebung angepaßt. Kleine Hummer agieren in der gleichen Weise wie die adulten. Die Wahl des Aufenthaltsplatzes und das Ausgraben der Löcher ist dem Verhalten sehr ähnlich, das vonHomarus americanus beschrieben worden ist. Die Art und Weise des Grabens erinnert auch an die vonNephrops norvegicus.

     

Spider assemblages in bird burrows

The arachnofauna of bird burrows, which are excavated in the soil, is incompletely understood. The bird burrows have a potential to serve as refugia for cavity-adopting spider species particularly in anthropogenic habitats formed by sand mining, which otherwise suffer from a limited availability of other types of cavities. We hypothesized that the presence of abundant food resources and safe shelter in bird burrows excavated in the soil allow the existence of specialized assemblage of spiders, similarly to those known from cavities and nests made by other birds and mammals. Here we examined 353 burrows that had been previously occupied by Riparia riparia, Merops apiaster or Passer montanus. The burrows were examined in early May and early September in 24 Czech sand pits and construction sites. The burrows hosted a species-rich assemblage of spiders that, however, occurred at low abundances. The spiders were represented prevalently by species known to have distributions centered in anthropogenic and urban habitats, including species that were never observed outside of heated buildings in the study area and species that only were previously known from mammalian burrows and loess and karstic soil crevices. Spider assemblages strongly differed between bird burrows and cavities and nests made by other birds and mammals. The species composition and overall low abundance of spiders in bird burrows was unexpected and was in strong contrast to previous observations of spider assemblages in cavities and nests made by other birds and mammals. Concluded, we rejected the initial hypothesis and, instead, we have shown that bird burrows are rarely occupied by spiders and if occupied, the spider species that adopt old bird burrows and the nests inside of them predominantly consist of species known to have their distribution centered to anthropogenic and urban habitats.     

Oxygen measurements in the burrows of freshwater insects

1. Thin-tipped micro-electrodes were used to measure oxygen concentrations in the burrows of two common aquatic insects, the mayfly Hexagenia limbata and the alderfly Sialis velata . Both species maintain their surroundings oxygenated by drawing water from above the sediment surface into their tubes. 2. The temporal pattern of oxygen in the burrows differed between the species. The constant high oxygen concentration (>75% of air saturation) measured in the tubes of the mayfly suggest that this animal pumps water almost continuously, which is consistent with its high oxygen requirements. In contrast, oxygen concentration in burrows of the alderfly fluctuated widely over time, suggesting that this animal irrigates only irregularly, probably because it can tolerate short periods of low oxygen concentration in its burrow. 3. The interval between pumping episodes by the alderfly decreased with increasing temperature, a result of increased oxygen consumption by the animal and by sediment at high temperature. 4. Based on the tube dimensions, oxygen penetration depth and animal density in lakes, we estimate that Hexagenia could create an oxic micro-environment equivalent to 3–35% of the volume of the surface oxidized sediment layer created by molecular diffusion. The mosaic of oxic micro-environments created by the burrowing and irrigation of freshwater animals could influence chemical and biological processes in sediments, the fluxes of materials between the sediment and the overlying water column, and the exposure of benthic animals to sedimentary contaminants.     

Partitioning of habitable pore space in earthworm burrows

Earthworms affect macro-pore structure of soils. However, some studies suggest that earthworm burrow walls and casts themselves differ greatly in structure from surrounding soils, potentially creating habitat for microbivorours nematodes which accelerate the decomposition and C and N mineralization. In this study aggregates were sampled from the burrow walls of the anecic earthworm Lumbricus terrestris and bulk soil (not altered by earthworms) from mesocosm incubated in the lab for 0, 1, 3, 5 and 16 weeks. Pore volumes and pore sizes were measured in triplicate with Mercury Intrusion Porosimetry (MIP). This method is well suited to establish pore size structure in the context of habitat, because it measures the stepwise intrusion of mercury from the outside of the aggregate into ever smaller pores. The progress of mercury into the aggregate interior thus resembles potential paths of a nematode into accessible habitable pore spaces residing in an aggregate. Total specific pore volume, V(s), varied between 0.13 and 0.18 mL/g and increased from 3 to 16 weeks in both burrow and bulk soil. Differences between total V(s) of bulk and burrow samples were not significant on any sampling date. However, differences were significant for pore size fractions at the scale of nematode body diameter.     

First observations of the burrows of Anguilla japonica

The burrow morphology of the Japanese eel Anguilla japonica was studied using in situ resin‐casting in a mud bottomed tidal drainage channel adjacent to the Fukui River in Tokushima, Japan. Two eels (62·5 and 56·3 cm total length) were initially fished from the burrows to verify that they were being used by A. japonica . Casts were made of 10 burrows that were found to have from one to three openings and main tunnels that were parallel to the axis of water flow in the channel. The maximum depths of the tunnels in the mud were 17·8–30·0 cm. The diameters of main tunnels ranged from 1·2 to 7·9 cm, were almost always wider than the bodies of the Japanese eels examined, and were more variable in the horizontal axis than in the vertical axis. There were no other animals capable of constructing a long and thin burrow in this channel, so these observations indicate that anguillids are able to construct their own burrows in soft mud sediments that may be used for extended periods of time.     

Clustered animal burrows yield higher spatial heterogeneity

An understanding of the relationships between spatial heterogeneity and disturbance regime is important for establishing the mechanisms necessary to maintain biodiversity. Our objective was to examine how the configuration of disturbance by burrowing rodents (Siberian marmot) affected the spatial heterogeneity of vegetation and soil nutrient properties. We established three 2500-m² (50 m × 50 m) isolated-burrows plots and three 2500-m² clustered-burrows plots in a Mongolian grassland. Each plot was subdivided into 4-m² quadrats, and the plant species richness, percent coverage, and soil nutrient properties in the quadrats were surveyed. Spatial heterogeneity was calculated for vegetation using the mean dissimilarity of species composition among sample quadrats, and geostatistical analysis was used to calculate soil properties. Heterogeneous patches of plants such as Achnatherum splendens and higher nutrient concentrations were found only near the clustered burrows. As a result, spatial heterogeneities of vegetation and soil nutrient properties were higher in the clustered colony than those in the isolated colony. The configuration of disturbance patches affected the spatial heterogeneity at the landscape level through the spatial pattern of disturbance frequency.     

Unusual nonmarine burrows from the Middle Jurassic of Scotland

The Kilmaluag Formation of the Great Estuarine Group (Middle Jurassic) of Scotland represents deposition of mixed carbonate and clastic sediments in a low‐salinity coastal lagoon to floodplain lake setting. Large, unusual trace fossils occur at two horizons within the formation. One type consists of platelike structures about 50 cm in diameter, which are found on wave‐rippled sandstone. These structures, strikingly similar to burrows produced by modern mudskippers, are assigned to fish that shallowly burrowed into the lagoon‐shore sediment.

The second type of burrows, found in brecciated, dolomitic limestones, are pipelike, about 4 to 7 cm in diameter and as much as 50 cm deep. One example has a chamber at the base of the pipe. Although most features of these structures appear similar to modern lungfish burrows, the chamber is most similar to structures produced by modern crayfish. The animal probably burrowed into the moist, mudflat sediment to escape desiccation during seasonal aridity.     

Infaunal burrows are enrichment zones for Vibrio parahaemolyticus

Vibrio parahaemolyticus, a species that includes strains known to be pathogenic in humans, and other Vibrionaceae are common, naturally occurring bacteria in coastal environments. Understanding the ecology and transport of these organisms within estuarine systems is fundamental to predicting outbreaks of pathogenic strains. Infaunal burrows serve as conduits for increased transport of tidal waters and V. parahaemolyticus cells by providing large open channels from the sediment to salt marsh tidal creeks. An extensive seasonal study was conducted at the North Inlet Estuary in Georgetown, SC, to quantify Vibrionaceae and specifically V. parahaemolyticus bacteria in tidal water, fiddler crab (Uca pugilator, Uca pugnax) burrow water, and interstitial pore water. Numbers of V. parahaemolyticus bacteria were significantly higher within burrow waters (4,875 CFU ml(-1)) than in creek water (193 CFU ml(-1)) and interstitial pore water (128 CFU ml(-1)), demonstrating that infaunal burrows are sites of V. parahaemolyticus enrichment. A strong seasonal trend of increased abundances of Vibrionaceae and V. parahaemolyticus organisms during the warmer months of May through September was observed. Multilocus sequence typing (MLST) analysis of isolates presumed to be V. parahaemolyticus from creek water, pore water, and burrow water identified substantial strain-level genetic variability among V. parahaemolyticus bacteria. Analysis of carbon substrate utilization capabilities of organisms presumed to be V. parahaemolyticus also indicated physiological diversity within this clade, which helps to explain the broad distribution of these strains within the estuary. These burrows are "hot spots" of Vibrionaceae and V. parahaemolyticus cell numbers and strain diversity and represent an important microhabitat.     

不同放牧模式下高原鼠兔洞口的空间分布格局变化

2019年4-11月,在四川省若尔盖县选取全年禁牧、冬季放牧、全年放牧3种放牧模式样地,对高原鼠兔(Ochotona curzoniae)洞口的数量、空间分布格局变化及影响因子进行了研究.计算平均最近邻指数和S2/m比值来分析样方(10m×10m)和样地水平下的空间分布格局,通过非参数检验评估空间分布格局在不同放牧模式...     

Ecology of spiders inhabiting abandoned mammal burrows in South African savanna

Summary We marked the sites chosen by 338 foundress queens of two desert ant species (Veromessor pergandei and Myrmecocystus flaviceps) and monitored changes in the spacing of both species and the foraging activity at V. pergandei young nests. Although the long established colonies of both species tend intraspecifically toward regular dispersion, queens of both species were intraspecifically clumped. After 3 months, when the first workers emerged, the young colonies (reduced to a total of 42 colonies) were randomly spaced intraspecifically. We also followed the spatial patter of queens with respect to established colonies of both species. Queens founded nests away from the nests of all established colonies on the site. After three months, the young colonies were dispersed away from conspecifics only. During June through August 1986, we censused the number of foragers at the surviving V. pergandei nests. Young colonies that were more active also tended to be far from established conspecifics in July and August. There was no correlation of forating activity with distance to heterospecific established colonies in any month. These results indicate that established conspecifics may reduce the survivorship of young ant colonies.     

Scoyenia burrows from Ordovician palaeosols of the Juniata Formation in Pennsylvania

Scoyenia beerboweri is a new ichnospecies of burrow from the late Ordovician (Ashgill) Juniata Formation in central Pennsylvania, USA. The burrows are abundant in red calcareous palaeosols, and were created by animals living at the time of soil formation, because they are filled with red sediment like that of the palaeosol matrix, and both cut across, and are cut by, nodules of pedogenic carbonate. The isotopically light carbon and oxygen of carbonate in the palaeosols indicate a terrestrial ecosystem of well-drained floodplains in a tropical seasonally-dry semi-arid palaeoclimate. Backfill layering within the burrows is evidence of a bilaterally symmetrical animal. Size distribution of the burrows reveals discontinuous growth, as found in arthropods. Ferruginized faecal pellets in the burrows indicate that they ingested sediment. For these reasons the burrows of Scoyenia beerboweri are most likely to be the work of millipedes. The nature of vegetation supporting them is unknown, although a single problematic plant-like fossil cast was found, and liverwort spores are widespread in rocks of this age. Vegetative biomass was limited judging from the degree of chemical weathering, extent of burial gleization and isotopic composition of carbon in the palaeosols. These distinctive respiration-dominated liverwort-millipede polsterlands lived at a time of global greenhouse climate, following Precambrian–Cambrian lichen-algal microbial earths and supplanted by Silurian brakelands of early vascular land plants.     

The bulk hydraulic conductivity of mangrove soil perforated with animal burrows

Flow of groundwater from mangrove swamp sediment to mangrove creeks is likely to be an important pathway in mangrove swamps, particularly for the removal of salt excluded at the mangrove root. The swamps are generally saturated with water, and are perforated with animal burrows, allowing significant groundwater flow to mangrove creeks to occur. The hydraulic conductivity of the sediment is thus an important physical parameter but is very difficult to measure in-situ. In this work, we describe a simple method for determining the hydraulic conductivity of mangrove sediment, including the effect of macropores such as crab burrows, which uses the existing animal burrows as piezometers. Experiments to measure the hydraulic conductivity of the sediment were carried out in a variety of mangrove forests. It was found that hydraulic conductivity varied from around 1 to 10 m per day, which is at least 10 times greater than would be expected if there were no burrows. In order to check the validity of the method, conventional piezometers were used to determine the free water table level in an area of mangroves fringing a creek. From these measurements, hydraulic conductivity was determined independently and found to be consistent with the new methodology.