Daily accumulation rates of floating debris and attached biota on continental and oceanic island shores in the SE Pacific: testing predictions based on global models.

Background: Long-distance rafting on anthropogenic marine debris (AMD) is thought to have a significant impact on global marine biogeography and the dispersal of non-indigenous species. Therefore, early identification of arrival sites of AMD and its epibionts is crucial for the prioritization of preventive measures. As accumulation patterns along global coastlines are largely unstudied, we tested if existing oceanographic models and knowledge about upstream sources of litter and epibionts can be used as a simple and cost-efficient approach for predicting probable arrival sites of AMD-rafting biota in coastal zones. Methods: Using the Southeast Pacific as a model system, we studied daily accumulation rates, composition, and minimum floating times of AMD with and without epibionts on seven sandy beaches, covering the oceanic environment (Rapa Nui/Easter Island) and three regions (south, centre, north) along the Chilean continental coast, over a minimum of 10 consecutive days, and we contrast our results with predictions from published models. Results: Total AMD accumulation rates varied from 56 ± 36 (mean ± standard deviation) to 388 ± 433 items km-1 d-1 and differed strongly between regions, in accordance with local geomorphology and socioeconomic conditions (presence of larger cities and rivers upstream, main economic activities, etc.). Daily accumulation of items with pelagic epibionts (indicators of a pelagic trajectory) ranged from 46 ± 29 (Rapa Nui) to 0.0 items km-1 d-1 (northern continental region). Minimum floating times of rafts, as estimated from the size of pelagic epibionts, were longest in the South Pacific Subtropical Gyre's (SPSG) centre region, followed by the high-latitude continental region under the influence of the onshore West Wind Drift, and decreased along the continental alongshore upwelling current, towards lower latitudes. Apart from pelagic rafters, a wide range of benthic epibionts, including invasive and cryptogenic species, was found on rafts at the continental beaches. Similarly, we present another record of local benthic corals Pocillopora sp., on Rapa Nui rafts. Discussion: Our results agree with the predictions made by recent models based on the prevailing wind and surface current regimes, with high frequencies of long-distance rafting in the oceanic SPSG centre and very low frequencies along the continental coast. These findings confirm the suitability of such models in predicting arrival hotspots of AMD and rafting species. Moreover, storm surges as well as site-related factors seem to influence AMD arrival patterns along the Chilean continental coast and might cause the observed high variability between sampling sites and days. Our results highlight the possible importance of rafting as a vector of along-shore dispersal and range expansions along the SE Pacific continental coast and add to the discussion about its role in benthic species dispersal between South Pacific oceanic islands.

Morphology of ctenostome bryozoans: 6. Amphibiobeania epiphylla.

Ctenostome bryozoans are unmineralized and mostly marine. Their lack of calcified skeletal features requires other characters to be considered for systematic and phylogenetic considerations. As a continuation of an ongoing series of studies, we herein investigate the morphology of Amphibiobeania epiphylla, a unique bryozoan inhabiting mangrove leaves that are highly exposed to tidal cycles and regular dry events according to the tidal cycle. Besides this interesting mode of life, the species was originally interpreted to be a weakly mineralized cheilostome bryozoan, whereas molecular data place it among ctenostome bryozoans. To elucidate the systematic and phylogenetic position of the genus and also find morphological adaptations to an extreme habitat, we investigated the morphology of A. epiphylla in detail. Zooids show a lophophore with eight tentacles and a simple gut with a prominent caecum, lophophoral anus and most notably a distinct gizzard in the cardiac region. Gizzard teeth are multiple, simple homogeneous cuticular structures. The cuticle of the zooid is rather uniform and shows no respective thickenings into opercular flaps or folds. Likewise, apertural muscles are represented by a single pair of muscles. There are no specific closing muscles in the apertural area like the operculum occlusors of cheilostomes. Most prominent within zooids is a spongiose tissue filling most of the body cavity. Although not properly understood, this tissue may aid in keeping animals moist and hydrated during prolonged dry times. In summary, all morphological characters support a ctenostome rather than a cheilostome affinity, possibly with Vesicularioidea or Victorelloidea. In addition, we provide new molecular data that clearly supports such a closer relationship.

Substratum and morphometric relationships in the bryozoan genus Odontoporella, with a description of a new paguridean-symbiont species from New Zealand.

Members of the bryozoan family Hippoporidridae have frequently been found encrusting gastropod shells inhabited by hermit crabs, with which they appear to enter into a symbiotic relationship-shells occupied by hermits may in some species have a tubular extension of the encrusting bryozoan from the shell opening, induced by the presence of the crab. Such colony growth is characteristic of some species of Hippoporidra Canu and Bassler and Odontoporella Héjjas. The type species of Odontoporella, O. adpressa (Busk), has been attributed a nominal distribution from Chiloe Island, Chile (the type locality), to the Falkland Islands, New Zealand, and New Caledonia. In New Zealand, colonies are relatively easily obtainable from some localities, so a study was undertaken to ascertain substratum and morphometric relationships across the range of distribution of the species, using museum specimens and, where possible, fresh material. It became clear that the New Zealand population constitutes a separate species, here named O. bishopi n. sp., in which the orifice is proportionately larger than in O. adpressa. In contrast to O. adpressa, which settles on a range of substrata, O. bishopi preferentially settles on gastropod shells occupied by hermit crabs (mostly Paguristes setosus (H. Milne Edwards)) and shows sexual dimorphism at the level of the polypide. Male polypides not only have modified lophophores but also reduced guts.

Living and fossil Steginoporellidae (Bryozoa: Cheilostomata) from New Zealand.

The cheilostome bryozoan family Steginoporellidae in New Zealand comprises seven living species of Steginoporella. Three of these are new to science-Steginoporella discors n. sp., Steginoporella lineata n. sp. and Steginoporella modesta n. sp.-and one (Steginoporella magnifica) additionally occurs as a Plio-Pleistocene fossil. A new Early Pleistocene fossil species, Steginoporella tiara n. sp., is also recognised. The living species exhibit the full range of colonial morphologies known for the genus, and two of the new deep-shelf taxa described herein have the smallest known colonies, both linear, not exceeding 5 mm in width and 22 mm in length. One species has a recorded depth range down to 615 m, apparently the deepest known for the genus. Zooidal proportions vary, with a length:width ratio in the seven living species ranging from 1.31 to 1.81, exceeded only by that in the new fossil taxon, which has very elongate zooids. Notwithstanding the conspicuous differences in colonial and zooidal morphology, four of the living species appear to be closely related, sharing distinctive reticulation of opercular sclerites, a similar morphology of the median process and no B-zooid morphs. Only one New Zealand taxon has B-zooids. Biogeographically, all the species except S. magnifica (also known from Tonga) are nominally endemic, but it is possible that some of the deeper-water taxa may eventually be found outside the boundary of the New Zealand Exclusive Economic Zone. The operculum in Steginoporella species is initially a single thin layer continuous with the membranous frontal wall, becoming two-layered when fully functioning in feeding zooids and mandibulate B-zooids.