Action of polyvalent cations on sodium transport across skin of larval and adult Rana catesbeiana

Developmental and evolutionary history affect survival in stressful environments

The world is increasingly impacted by a variety of stressors that have the potential to differentially influence life history stages of organisms. Organisms have evolved to cope with some stressors, while with others they have little capacity. It is thus important to understand the effects of both developmental and evolutionary history on survival in stressful environments. We present evidence of the effects of both developmental and evolutionary history on survival of a freshwater vertebrate, the rough-skinned newt (Taricha granulosa) in an osmotically stressful environment. We compared the survival of larvae in either NaCl or MgCl2 that were exposed to salinity either as larvae only or as embryos as well. Embryonic exposure to salinity led to greater mortality of newt larvae than larval exposure alone, and this reduced survival probability was strongly linked to the carry-over effect of stunted embryonic growth in salts. Larval survival was also dependent on the type of salt (NaCl or MgCl2) the larvae were exposed to, and was lowest in MgCl2, a widely-used chemical deicer that, unlike NaCl, amphibian larvae do not have an evolutionary history of regulating at high levels. Both developmental and evolutionary history are critical factors in determining survival in this stressful environment, a pattern that may have widespread implications for the survival of animals increasingly impacted by substances with which they have little evolutionary history.

Ground water chemistry changes before major earthquakes and possible effects on animals

Prior to major earthquakes many changes in the environment have been documented. Though often subtle and fleeting, these changes are noticeable at the land surface, in water, in the air, and in the ionosphere. Key to understanding these diverse pre-earthquake phenomena has been the discovery that, when tectonic stresses build up in the Earth’s crust, highly mobile electronic charge carriers are activated. These charge carriers are defect electrons on the oxygen anion sublattice of silicate minerals, known as positive holes, chemically equivalent to O⁻ in a matrix of O²⁻. They are remarkable inasmuch as they can flow out of the stressed rock volume and spread into the surrounding unstressed rocks. Travelling fast and far the positive holes cause a range of follow-on reactions when they arrive at the Earth’s surface, where they cause air ionization, injecting massive amounts of primarily positive air ions into the lower atmosphere. When they arrive at the rock-water interface, they act as •O radicals, oxidizing water to hydrogen peroxide. Other reactions at the rock-water interface include the oxidation or partial oxidation of dissolved organic compounds, leading to changes of their fluorescence spectra. Some compounds thus formed may be irritants or toxins to certain species of animals. Common toads, Bufo bufo, were observed to exhibit a highly unusual behavior prior to a M6.3 earthquake that hit L’Aquila, Italy, on April 06, 2009: a few days before the seismic event the toads suddenly disappeared from their breeding site in a small lake about 75 km from the epicenter and did not return until after the aftershock series. In this paper we discuss potential changes in groundwater chemistry prior to seismic events and their possible effects on animals.

Morphology of ventral epidermis of Rana catesbeiana during metamorphosis

A detailed morphological examination of the bullfrog tadpole ventral epidermis and changes in structure that occur during metamorphosis has not been done. Knowledge of this is crucial to interpretation of physiological studies such as those dealing with development of transepithelial Na+ transport. Examination of tadpole epidermis with light microscopy reveals the presence of three different cell types: apical, basal, and skein. This epidermal morphology is constant until Taylor and Kollros (Anat. Rec. 94:7-23, 1946) stage 19 when degeneration of apical cells is noted. Stages 20 and 21 are characterized by rapid proliferation of basal cells and development of a true stratum germinativum together with the disappearance of other tadpole cell types. By stage 22, epidermal morphology is similar to that of the adult frog. Studies with the electron microscope reveal that as the proliferation proceeds during metamorphosis, the skein cells, at stage 20, differentiate to form the apical border of the skin. The development of the adult frog cell phenotype appears to mimic the cellular differentiation that occurs in the adult epidermis with the cells first developing into progranular cells in the intermediate stratum of the skin and then progressing to granular cells in the outermost living cell layer. The granular cells then undergo cornification to form the stratum corneum. Mitochondria rich cells are not seen in the developing epidermis until stage 21. These observations, when considered with previous results from Na+ transport studies (Hillyard et al.: Biochim. Biophys. Acta 692:455-461, 1982), suggest that both the physiological differentiation and morphological differentiation are simultaneous events.