Austinogebia, a new genus in the Upogebiidae and rediagnosis of its close relative, Gebiacantha Ngoc-Ho, 1989 (Crustacea: Decapoda: Thalassinidea)

New material described recently permits the separation of six upogebiid species into the new genus Austinogebia, for which the diagnostic characters and a key are presented. The new taxon is compared to its close relative, Gebiacantha Ngoc-Ho, 1989, and the opportunity is taken to rediagnose the latter.     

The effects of temperature and salinity on ventilation behavior of two species of ghost shrimp (Thalassinidea) from the northern Gulf of Mexico: a laboratory study

Thalassinidean shrimp are among the most important bioturbators in coastal ecosystems. The species Lepidophthalmus louisianensis and Callichirus islagrande are found in dense aggregations (up to 400 burrows m⁻²) along sandy and muddy shores of the northern Gulf of Mexico. These shrimp actively ventilate their burrows to provide oxygen and eliminate wastes. In doing so, they expel nutrient-rich burrow water to the overlying water column, potentially altering nutrient cycling and benthic primary productivity. To develop a mechanistic understanding of the role of burrowing shrimp in nutrient processes, we must first examine how changes in environmental conditions alter the frequency, strength, and duration of ventilation. Field measurements of burrow temperature and salinity suggest that the burrow serves as a buffer from the highly variable conditions found in these estuarine, intertidal habitats. Temperatures at sediment depths >30 cm were generally warmer in winter and cooler in summer than at the sediment surface. Burrow salinities, measured at low tide, were consistently higher than adjacent open water. We used these measurements to parameterize laboratory studies of burrow ventilation in artificial burrows made of plastic tubing and in more natural sediment mesocosms, and studies of oxygen consumption in small glass containers. Rates of oxygen consumption and burrow ventilation by L. louisianensis were lower than those of C. islagrande, perhaps reflecting a lower overall activity rate in the former species which resides in less permeable sediments. Generally, increased temperature had a significant positive effect on oxygen consumption for both species. Salinity had no effect on oxygen consumption by L. louisianensis, reflecting the ability of this species to exist in a wide range of salinities. In contrast, oxygen consumption rates of C. islagrande, which is less tolerant of low salinity, were significantly higher at 35‰ than at 20‰. Ventilation rates were highly variable, and shrimp in artificial burrows tended to have consistently higher ventilation rates than those in sediment mesocosms. There is a trend toward more frequent ventilation at 30 °C for both species. Salinity had no effect on ventilation for either species. Our results suggest that thalassinideans exhibit highly variable and species-specific ventilation patterns that are more likely to be affected by temperature than salinity. Increased ventilation at higher temperatures seems to coincide with increased oxygen consumption at these temperatures, although a similar finding was not made for salinity treatments.     

A modern analogue for the trace fossil Gyrolithes: burrows of the thalassinidean shrimp Axianassa australis

The tidal flats at Praia do Araça, Brazil have muddy siliciclastic sediments on the surface and a layer of heavily packed shells down to 30–40 cm depth. The most obvious element of the infauna is the thalassinidean shrimp Axianassa australis. Several animals were captured with a yabby pump. Burrow openings were characterized by a low mound (1-2 cm high and 10–30 cm in diameter at the base) with one or two simple holes nearby (20-70 cm away). Counts along two transects showed a mean density of Axianassa burrow openings of 1.4 m⁻² (range: 0–7), mounds ranged in density from 0 to 3 m⁻² (mean 1.25). Three nearly complete (and several incomplete) resin casts showed a unique burrow shape, with spiral shafts leading to wide horizontal galleries from which several evenly proportioned corkscrew-shaped spirals branched off, leading to further horizontal galleries at greater sediment depths. Burrows had up to 15 such spirals and a total length of over 8 m. The total burrow depth was between 106 and 130 cm. The role of the spirals and the similarity of Axianassa burrows to the trace fossil Gyrolithes are discussed.     

Nutritional ecology of thalassinidean shrimps constructing burrows with debris chambers: The distribution and use of macronutrients and micronutrients

Four different approaches were combined to determine the nutritional relevance of debris chambers in the burrows of two thalassinidean shrimps: (1) the natural abundance of carbon and nitrogen stable isotopes in potential food sources, (2) their nutritional value based on the content and composition of essential nutrients, (3) a dual labelling experiment with shrimp in aquaria employing ¹⁵N- and ¹³C-labelled seagrass debris and (4) ration estimates using the acquisition rate of plant debris by the shrimps. The results of the four approaches confirmed the use of plant debris as a food source. Based on the natural abundance of stable isotopes, Corallianassa longiventris apparently relies on the chamber content and the burrow wall as sources of carbon and nitrogen, whereas Pestarella tyrrhena probably relies on ambient debris and on benthic foraminiferans and microphytobenthos in the surface sediment. Corallianassa longiventris obtains its essential nutrients predominantly from chamber debris and to a lesser extent from its burrow wall, P. tyrrhena from chamber debris, the burrow wall and the surface sediment. Among the essential nutrients, those amino acids commonly deficient to deposit feeders were particularly enriched in the burrow environments of the two shrimps. Highly unsaturated fatty acids (HUFAs) were lacking in all of C. longiventris potential food sources; this species may either be able to synthesize them de novo from linolic acid or may use another unknown source. For P. tyrrhena, surface sediment and chamber debris represent potential HUFA sources. The most probable thiamine and β-carotene supplier for C. longiventris is the chamber debris, for P. tyrrhena again the surface sediment. In both species, the rate of debris introduction into the burrow is sufficient to meet the nutritional demand.     

中国南海阿蛄虾科一新种(甲壳纲:十足目:蝼蛄虾总科)

报道中国南海阿蛄虾科一新种,即董氏丽阿蛄虾Ｃａｌａｘｉｕｓ ｔｕｎｇｉ ｓｐ．ｍｏｖ．,对其形态特征作了描述,并与近似种进行了比较。     

Paleocene Thalassinidea colonization in deep-sea environment and the coprolite Palaxius osaensis n. ichnosp. in Southern Costa Rica

Palaxius osaensis n. ichnosp., a new ichnospecies of crustacean coprolite is described. The coprolite is preserved in a 200-m thick Paleocene sequence in Southern Costa Rica that is largely dominated by pillow basalts. The studied sample is part of a seamount formed in the Pacific Ocean that was accreted to the Central American isthmus during the Eocene. The absence of lava vesicles, shallow-water deposits, and detrital sediments in the section suggest that the coprolites were deposited in a deep environment during the first stage of the development of the seamount. This represents one of the deepest occurrences of Thalassinidea coprolites reported in the literature and indicates that the producers of the coprolites, presumably some shrimps, developed the aptitude to colonize abyssal environments at least since Early Tertiary. The crustacean coprolites were encountered at a site which apparently lacked a food supply, although hydrothermal processes are believed to have provided the opportunity for a chemotrophic community to develop on the deepest part of the seamount. P. osaensis n. ichnosp. is also found in Colombia in late Cretaceous shallow-water sediments that notably contain Palaxius caucaensis coprolites (Micropaleontology 41 (1995) 85-88). Occurrences of P. osaensis n. ichnosp. deposited at both shallow and deep levels may possibly be related to an aptitude of some thalassinid organisms to have developed in various biotopes during the late Cretaceous-Paleocene.