Freshwater reservoir ages and a potential freshwater diet effect are examined for Manitoba (Canada), using paired samples of contemporaneous terrestrial, freshwater, and omnivore-diet species (Homo sapiens, Gavia sp.). The freshwater diet effect (n=4) varies from 220 to 370 14C years. The FRE (n=12) is temporally variable, with a median of 230 14C years and values up to 880 14C years (or more). Understanding the FRE is important for geologists who reconstruct the postglacial history of an area. It is also important for archaeologists who rely on 14C dating to develop cultural histories, as inhabitants of the Canadian boreal forest have relied upon freshwater resources as a part of their diet. An analysis of the δ13C on 93 freshwater mollusk samples from 11 species demonstrates significant variability, which highlights the difficulty in assigning an “assumed” fractionation correction.

Our ability to reliably use radiocarbon (14C) dates of mollusk shells to estimate calendar ages may depend on the feeding preference and habitat of a particular species and the geology of the region. Gastropods that feed by scraping are prone to incorporation of carbon from the substrate into their shells as evidenced by studies comparing the radiocarbon dates of shells and flesh from different species on different substrates (Dye 1994; Hogg et al. 1998). Limpet shells (Patella sp.) are commonly found in prehistoric midden deposits in the British Isles and elsewhere, however these shells have largely been avoided for radiocarbon dating in regions of limestone outcrops. Results from limpets (Patella vulgata) collected alive on limestone and volcanic substrates on the coasts of Ireland indicate that the shells were formed in equilibrium with the seawater, with no significant 14C offsets. Limpets collected from the east coast of Northern Ireland have elevated 14C due to the output of Sellafield nuclear fuel reprocessing plant. In all locations, the flesh was depleted in 14C compared to the shells. The results will have an important consequence for radiocarbon dating of midden deposits as well as the bone of humans and animals who fed on the limpets.

Sediments containing terrestrial and aquatic mollusks and ostracodes from the Ziegler Reservoir fossil site (2705 m elevation) near Snowmass Village, Colorado, span ~130–87 ka (MIS 5e through 5b). The southeastern area of the site where taxa were recovered was a relatively fresh, shallow, well-vegetated wetland during MIS 5e through 5c time, approximately 2 m deep, with a total dissolved solids value of ~200–1000 mg L− 1. The wetland was seasonally or annually variable and groundwater discharged along the margins of the bounding moraine. Groundwater likely contributed solutes to the system and may have contributed 18O-enriched water. Based on stable isotopes from ostracode calcite (δ18OOST and δ13COST), seasonal evaporation occurred and the dissolved inorganic carbon pool was unexpectedly enriched in 13C. The mollusk and ostracode faunas changed little across the MIS 5e/5d/5c boundaries, whereas a distinct change in the ostracode fauna occurred between the deposition of Unit 11 and Unit 13, which corresponds in time to the MIS 5c/5b boundary, indicating some combination of increased surface and/or groundwater flow, a decrease in water temperature, and a freshening and a possible deepening of the wetland.

Multivariate analyses applied to Pleistocene bivalve assemblages from the Oga Peninsula (northern Japan) discriminate three distinct assemblages. The assemblages and their taphonomy were used to recognize environmental settings and changes. The Astarte–Cyclocardia–Glycymeris assemblage indicates shelf environment (below the storm wave base) where gravels and shells are transported from shallower settings. Supply of the exotic coarse sediment probably enabled epifaunal bivalves to inhabit the sea floor. The Glycymeris assemblage is characterized by dominance of G. yessoensis and represents current-swept shoreface environment (above the storm wave base). The Moerella assemblage is characterized by bivalves inhabiting bay to open-marine conditions and diverse deposit-feeders, indicating a moderately land-locked environment, such as an open bay or a bay mouth. Fine-grained substrata rich in organic matters in the bay were probably suitable for the deposit-feeders. Ordination also shows the assemblages along two environmental gradients, a bathymetrical one and the other related to open-marine and bay conditions. The environmental changes are explained mainly by glacio-eustatic sea-level changes and alternation of coastal geomorphology caused by local crustal movements. This study also suggests that fossil assemblages can be a powerful tool to reconstruct environments and depositional dynamics even in intensely bioturbated sedimentary facies.

We quantified Δ14C, δ18O, and δ13C cycles along ontogeny within four bay scallop (Argopecten purpuratus) shells collected from Callao Bay, Salaverry, and Sechura Bay, Peru following the 1907–1908 non-El Niño years and the 1925–1926 El Niño. Δ14C and δ13C generally covary; Δ14C and δ18O vary inversely. Simultaneous decreases in Δ14C and increases in δ18O in non-El Niño shells are followed by constant Δ14C and gradually decreasing δ18O, which we interpret as evidence for discrete marine upwelling events followed by warming of the initially cold upwelled water. Upwelling changes from El Niño events are detectable with difficulty in mollusk shell Δ14C.

Intracellular recording in the retina of the snail, Helix pomatia L., reveals the existence of two types of cell responsive to diffuse flashes of achromatic or monochromatic light: B-type cells, which respond with sustained depolarization that is sometimes accompanied by spikes, and D-type cells, which respond with sustained hyperpolarization. The peak of spectral sensitivity for both B- and D-cells falls in the 450-500 nm range and coincides with range of maximal sensitivity for the rhodopsin family of photopigments. Within a proposed two-channel model of snail achromatic vision, responses of the B- and D-cells are represented by a two-dimensional ‘excitation vector’. The length of the ‘excitation vector’ is approximately constant, and its direction correlates with light intensity. The vector model of light encoding in the snail is discussed in relation to models of achromatic vision in vertebrates (fish, frog, monkey, and humans) based on psychophysical, behavioral and neurophysiological data. Intracellular data in the snail taken together with data from vertebrate animals support the hypothesis that a 2-dimensional model of brightness and darkness encoding utilizes a universal mechanism of ‘vector encoding’ for light intensity in neuronal vision networks.

The aim of our study was to distinguish the stress-related molecular response of thepulmonate mollusc Lymnaea stagnalis from the Chernobyl area in comparisonwith the consequences of other harmful effects, including the short-term effects ofradiation and heating. Specimens inhabiting ponds near the Chernobyl nuclear power plant,the cooling channel of the electric power station and the soil-reclamation channel (groupsR, T and C, correspondingly), and specimens adapted to laboratory conditions (a controlgroup (CL), a disposable group exposed to 2 mGy X-ray radiation over the body (RL), and agroup exposed to 25 °C for 4 days (TL)) were compared. Despite high variability ofresponses, Principle Component Analysis distinctly separated the laboratory and feralgroups into two sets. In the feral groups, low levels of the stress-related andmetal-binding protein metallothionein (MT), protein carbonyls and lactate dehydrogenase inthe digestive gland were indicated. The main separating criteria selected byclassification and regression tree analysis were the protein carbonyls, cholinesterase andMT. Molluscs from group R were clearly distinguished by the lowest levels of MT,Mn-superoxide dismutase and lactate dehydrogenase, and the highest level of glutathione,demonstrating that the oppression of the gene-determined stress-related response and itspartially metabolic compensation can be possible markers for chronic environmental effectsof irradiation.