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1.
The passage of a radio-opaque meal was followed through the digestive system of the red rock crab, Cancer productus, using a fluoroscope. When the crabs were maintained in seawater, the food was apparent in the foregut as soon as the animals had fed. Release of food from the foregut was routinely slow and digesta appeared in the midgut only in small amounts at any one time. The foregut was emptied between 24 and 36 h, digesta was cleared from the midgut region at 36 h and by 48 h only a small amount of residual digesta was left in the posterior part of the hindgut. Contractions of the cardiac region of the foregut were somewhat sporadic and ranged between 6 and 11 min-1. Contractions of the pyloric region were more stable, varying between 45-65 min-1. In both cases, there was no change in rate during 18 h period in seawater. When crabs were subjected to both short- and long-term aerial exposure, release of food from the foregut was halted for the first 4-6 h of emersion. Although, small amounts of digesta appeared in the midgut and hindgut, there was no significant change in the amount in each region during emersion. There was a trend towards a depression of cardiac stomach contraction rates, but this was only significant in 3 h postprandial crabs during short-term emersion. A pronounced decrease in pyloric stomach contraction rate was maintained for the duration of the aerial exposure. When crabs were returned to seawater, contraction rates took 3-5 h to return to normal, but no significant change in gastric evacuation was observed during this period. During re-immersion, over 65% of the animals regurgitated the stomach contents. This regurgitation may act as a protective mechanism to avoid digestion and the subsequent specific dynamic action. The decrease in gastric processing in C. productus is probably part of an overall metabolic depression occurring during emersion.  相似文献   
2.
African catfish Clarias gariepinus (=119.9&30.6 g) were exposed to periods of emersion (5, 30, 60, 90 and 180 min) and the ammonia and nitrogen excretion rates measured following re-immersion. Immediately following re-immersion (0–30 min), the ammonia excretion and relative ammonia excretion was greatest for the 5-min emersion gro up. Exposure to extended periods of emersion resulted in a decrease in total nitrogen excretion, notably ammonia excretion, although no significant changes were observed in the non-ammonia component of C. gariepinus .  相似文献   
3.
In a global change context, the intensity and the frequency of drastic low flow periods or drought events will most likely increase to a substantial extent over the coming decades, leading to a modification in the abiotic characteristics of wetlands. This change in environmental parameters may induce severe shifts in plant and animal communities and the functioning of ecosystems. In this study, we experimentally estimated the effect of drought and the accumulation of ammonia (NH3) on the feeding activities of three generalist macroinvertebrates (i.e. Gammarus pulex, Gammarus roeselii and Asellus aquaticus) on three types of organic matter: leaves of Berula erecta growing in submerged conditions, leaves of the same species growing in emerged conditions and dead leaves of Alnus glutinosa. We observed a modification in the biomechanical and stoichiometric characteristics of the plants as a result of the emersion of the aquatic plants. This shift produced a substantial decrease in organic matter recycling by invertebrates and in their associated physiological ability (i.e. the energy stores of the animals) to face conditions associated with environmental change. Moreover, the accumulation of NH3 amplified the negative effect of emersion. This snowball effect on invertebrates may profoundly modify the functioning of ecosystems, particularly in terms of organic matter production/degradation and carbon mineralization.  相似文献   
4.
Laboratory experiments were conducted to investigate tolerance and physiological responses of Galaxias'nebula', a newly discovered and widespread African galaxiid, to aerial exposure. This species can tolerate emersion for at least 36 h. Changes in water level and dewatering did not induce the fish to burrow into the substratum or find refugia, nor was there detectable mucus production following aerial exposure. Opercular movement, a proxy for gill ventilation rate, however, did vary with changes in water level. The initial steady ventilation rate increased significantly when the fish were partially emersed and ventilation ceased immediately upon total air exposure. When fish were re-immersed, there was first a period of hyperactivity with a corresponding inflated gill ventilation rate which was restored to pretreatment levels within 2 h. This is the first documented case of amphibious capabilities in an African galaxiid, which has implications for the interpretation of its widespread distribution pattern.  相似文献   
5.
In Recent coral reefs, emersion has resulted in the development of special growth forms of colonial corals which have been named microatolls. These colonies grow almost exclusively in a horizontal direction. In the upper part of the colony, subaerial exposure leads to the decay of the living body. The growth then stops and the skeleton is later colonized by various boring and encrusting organisms. Here we show the first record of a massive Mesozoic coral colony displaying the main features of emersion. The colony has been collected in perireefal Oxfordian (Jurassic) limestones from the Jura Mountains (France). It is situated exactly at the expected place in a shallowing-upward sequence between infralittoral buildups and supralittoral limestones. We suggest that such growth structures could be more common than previously thought in ancient coralliferous sediments and add some new details to discriminate between these colonies.  相似文献   
6.
We hypothesised that the exploration tendency of the amphibious mangrove rivulus Kryptolebias marmoratus would be inhibited in the terrestrial environment because of constraints on terrestrial locomotion or orientation. Using a novel object test, we showed that the fish explored objects in the aquatic but not the terrestrial environment, supporting the existence of constraints on terrestrial exploration. In further tests of the effects of extrinsic factors on terrestrial movement between aquatic refuges, shallow water depth simulating desiccation risk and the presence of a conspecific simulating intraspecific competition increased emersion outside of refuges, while high water salinity had no effect. These extrinsic factors had little effect on terrestrial movement between different aquatic refuges, except possibly for the lowest water depth tested. A significant association observed between emersion activity and movement between aquatic refuges suggested that terrestrial movement in K. marmoratus might depend on the tendency of individuals to emerse.  相似文献   
7.
The Upper Cretaceous succession in the Madenli area (western Central Taurides, Southern Turkey) consists of platform carbonate rocks deposited in entirely peritidal environments, which are sensitive to sea level changes driven by global eustasy, but also strongly affected by local and regional tectonics. It includes economically important bauxite deposits. Previous works suggest different ages for bauxite formation ranging from the Albian to the Santonian. Benthic foraminiferal biostratigraphy and facies analysis of the Madenli and Doğankuzu outcrop sections allow for a more precise dating of the platform emersion periods. The footwall limestones of the bauxite deposits consist of well-bedded limestones (Unit-1), which contain a benthic foraminiferal assemblage (BFA) including mainly Biconcava bentori and Pastrikella biplana, Chrysalidina gradata (BFA I), assigned to the middle-upper Cenomanian. In the Madenli section, the first bauxite deposit occurs in the upper part of Unit-1 as a layer interbedded with pinkish sparitic and dolomitic beds (subunit-1a) deposited in supratidal environment. Subunit-1a is stratigraphically equivalent to the Doğankuzu and Mortaş bauxite deposits considered as karst-related, unconformity-type deposits. The hanging-wall limestones of the bauxite are represented by the massive limestones (Unit-2) starting locally with either the upper Cenomanian characterized mainly by the presence of Pseudolituonella reicheli or upper Campanian comprising mainly Murciella cuvillieri and Moncharmontia apenninica (BFA II). There is no field evidence of a discontinuity surface at the contact between the lower part of Unit-2, including BFA I, and the upper part of Unit-2, including BFA II. This contact is defined as a paraconformity indicating a stratigraphic gap from the Turonian to the early Campanian. The top of Unit-2 is truncated by another discontinuity surface associated with a minor bauxite deposit. The overlying Unit-3 is characterized by well-bedded, rudist-bearing limestones topped by laminated and dolomitized limestones organized in shallowing upward cycles. It is assigned to the upper Maastrichtian based on the presence of Rhapydionina liburnica (BFA III) and rudist assemblage. A third emersion period of the platform corresponds to the early Maastrichtian.  相似文献   
8.
The green shore crab, Carcinus maenas, undergoes on average 6?h periods of emersion during each low-tide cycle during the summer months. Under those conditions, the crab is cut off from its normal water environment and is exposed to potential stress from a suite of environmental and physiological changes: dehydration, compromised gas exchange and resultant internal hypoxia and hypercapnia, thermal stress, and ammonia toxicity. This study examined the comprehensive responses of the green crab in water and to a 6?h emersion period laboratory simulation of a tidal cycle followed by a 1?h re-immersion period, measuring indicators of dehydration, hemolymph osmolality, oxygen uptake, hemolymph acid–base status, heart and ventilatory rate, and hemolymph ammonia and ammonia excretion. Green crabs showed physiological responses of varying magnitude to 6?h of emersion. Individuals were found in the field exclusively under rocks and large clumps of seaweed where temperatures were approximately half those of exposed surfaces and relative humidity was about twice as high as ambient air. During emersion, crabs lost less than 5% of their wet weight, and hemolymph osmolality did not increase significantly. Oxygen uptake continued in air at about 50% of the control, aquatic values; and the gills continued to be ventilated by the scaphognathite, albeit at lower rates. Hemolymph lactate concentrations increased, indicating a shift to a greater reliance on anaerobic metabolism to support energetic needs. A slight acidosis developed in the hemolymph after 1?h of emersion, but it did not increase thereafter. Ammonia concentrations in the hemolymph were unchanged, as ammonia was volatilized by the gills and excreted into the air as NH3 gas. These results show that the green crab copes with emersion by seeking refuge in microhabitats that mitigate the changes in the physical parameters of intertidal emersion. Physiologically, desiccation is avoided, cardio-respiratory processes are maintained at reduced levels, and hemolymph acid–base balance is minimally affected. Ammonia toxicity appears to be avoided by a shift to excreting NH3 gas directly or indirectly to air.  相似文献   
9.
The effects on photosynthesis of CO2 and desiccation in Porphyra haitanensis were investigated to establish the effects of increased atmospheric CO2 on this alga during emersion at low tides. With enhanced desiccation, net photosynthesis, dark respiration, photosynthetic efficiency, apparent carboxylating efficiency and light saturation point decreased, while the light compensation point and CO2 compensation point increased. Emersed net photosynthesis was not saturated by the present atmospheric CO2 level (about 350?ml?m?3), and doubling the CO2 concentration (700?ml?m?3) increased photosynthesis by between 31% and 89% at moderate levels of desiccation. The relative enhancement of emersed net photosynthesis at 700?ml?m?3 CO2 was greater at higher temperatures and higher levels of desiccation. The photosynthetic production of Porphyra haitanensis may benefit from increasing atmospheric CO2 concentration during emersion.  相似文献   
10.
王龙乐  张鑫  邹定辉  陈斌斌 《生态学报》2017,37(22):7710-7717
在有性繁殖时期,潮间带海藻羊栖菜(Hizikia fusiformis)的叶状体与生殖托遭受低潮干出脱水的影响。为阐明羊栖菜在有性繁殖时期不同部位对干出脱水的耐受能力,研究了羊栖菜的叶状体和雌、雄生殖托在干出脱水过程中以及随后的沉水恢复状态下叶绿素荧光动力学参数变化。实验结果表明,羊栖菜叶状体及其生殖托的PS Ⅱ有效光化学量子产量[Y(Ⅱ)]分别在0—73%和0—60%的脱水率范围内未发生显著变化,而继续脱水则会显著降低藻体的Y(Ⅱ),表明羊栖菜叶状体和生殖托的Y(Ⅱ)下降的脱水界限值分别为73%和60%,对脱水耐受能力较强。在连续干出脱水过程中,叶状体和生殖托的最大相对电子传递速率(rETR_(max))和光强耐受能力(Ⅰ_k)都显著下降,且在严重脱水状态(失水率为75%)下,羊栖菜叶状体和雌、雄生殖托的Y(Ⅱ)分别比干出初始时降低了12%、31%和37%,且复水后其雌、雄生殖托的Y(Ⅱ)无法恢复,甚至持续降低。同时叶状体和生殖托的r ETR_(max)、Ⅰ_k和光能利用效率(α)都显著下降,说明严重脱水使藻体不同部位的PS Ⅱ反应中心受到了不可逆的损伤。在持续大幅度脱水过程(失水率高于60%)中及随后的沉水恢复过程中,比较藻体各部位的Y(Ⅱ)值发现,叶状体雌生殖托雄生殖托,表明严重脱水对雄生殖托的影响最大,对叶状体的影响最小。在有性生殖阶段,为了羊栖菜能有性繁殖成功,应避免藻体,尤其是生殖托经受到严重的干出脱水胁迫。  相似文献   
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