A Review of the Chemical Ecology of Antarctic Marine Invertebrates

The interdisciplinary field of marine invertebrate chemicalecology is relatively young, and particularly so in polar marineenvironments. In this review we present evidence that the incidenceof chemical defense in antarctic benthic marine invertebratephyla is widespread. Mechanisms of chemical defense have beendetected in antarctic representatives of the Porifera, Cnidaria,Brachiopoda, Tunicata, Nemertea, Mollusca and Echinodermata.This argues against earlier bio-geographic theories that predicteda low incidence of chemical defense in polar waters where levelsof fish predation are low. Selection for chemical defense inbenthic sessile and sluggish marine invertebrates is likelya response to an environmentally stable community shown to bestructured primarily by biotic factors such as predation andcompetition. Holoplankton and the eggs, embryos and larvae ofboth benthic and planktonic antarctic macroinvertebrates mayalso employ chemical defense to offset mortality during characteristicallyslow development and long life span where susceptibility topredation is seemingly high. While most research to date hasfocused on the role of secondary metabolites in mediating predation,it is likely that bioactive compounds in antarctic marine invertebratesalso serve roles as antifoulants and allelochemics. The diversityof bioactive metabolites detected to date in antarctic marineinvertebrates sets the stage both for continuing and for broadeningefforts to evaluate their functional and ecological significance.     

A defence of the calcichordates

Peterson (1994, Short Courses in Paleontology 7, Pal. Soc. & Univ. Tennessee; 1995, Lethaia 28 ) has claimed that the calcichordate theory of the origin of chordates can be dismissed on purely methodological grounds, without evaluating the anatomy of the calcichordates. He claimed this on the basis of his finding that the interrelationships for extant deuterostomes obtained by a PAUP analysis were not altered by including calcichordate fossils in the analysis, allegedly coded according to the anatomical interpretations of the calcichordate theory. This result, however, was due (1) to acceptance of dubious homologies among extant deuterostomes, (2) to reliance, when asserting that the fossils made no difference, on a majority-rule tree based on 13 equal-shortest trees; and (3) to the use of numerous multi-state characters in coding, which had the effect of denying, a priori , many of the homologies claimed by the calcichordate theory between fossil and extant forms. When these errors are corrected, a new PAUP analysis yields a tree consistent with the calcichordate theory. Peterson's claim therefore fails.     

Elevation of Serum Dopamine-β-hydroxylase Activity with Forced Immobilization

THE formation of the neurotransmitter noradrenaline from 3,4-dihydroxyphenylethylamine (dopamine) is catalysed by the enzyme dopamine-β-hydroxylase (DBH)¹. This enzyme is associated both with the catecholamine-containing chromaffin granules in the adrenal medulla^2,3 and with the vesicular structures in sympathetic nerve terminals which contain catecholamines⁴. Furthermore, DBH activity is released with catecholamines into the perfusate after stimulation of either the isolated perfused adrenal gland⁵ or the isolated perfused spleen^6–8. DBH activity has been reported in the serum of both man and the rat^9,10. This activity is similar to adrenal and sympathetic nerve DBH activity with regard to cofactor requirements, oxygen requirement and kinetic characteristics^9,10. It has been suggested that serum DBH activity might be present as a result of release of enzyme with catecholamines from the adrenal glands and sympathetic nerves. If this is the case, serum DBH activity might be a useful and convenient index of sympathetic-adrenal activity. The work described here was undertaken to investigate both the source of the serum DBH and the effect on this activity of forced immobilization, a procedure which has been used as a model of stress and which has been shown to release catecholamines from the adrenal gland and increase catecholamine excretion¹¹.     

Janospira - an Ordovician microfossil in search of a Phylum

Janospira is described from early Ordovician (Arenig) rocks of northern Spitsbergen. It is a curious microfossil, probably calcareous, about 1 mm in length, made up of an initial coil which expands distally into a straight tube, at the same time as producing a narrower tube almost in line with the first but in the opposite direction. Although showing some similarities to Foraminifera, molluscs and polychaetes, there are objections to its inclusion in any of these groups, and it is equally probable that it belongs to an unknown group with a planktic early growth stage.     

A revised ammonite zonation of the Boreal Oxfordian and its application in northeast Greenland

A revised ammonite zonation for use in the Middle–Upper Oxfordian of the Boreal province is put forward. The zonation is used to date late Jurassic sediments in the Wollaston Forland area of northeast Greenland. The sediments broadly comprise basinal mudstones and shallow marine and shoreline sandstones, which were deposited in westerly tilted fault blocks during three transgressive pulses. On the peneplaned surfaces of wide tilted fault blocks a thick sequence of tidally and fluvially influenced marine sandstones of Middle Jurassic age was deposited. In the Upper Jurassic deposition initially took place in the centre of the basin where 80 m of shoreface sandstones accumulated (Jakobsstigen Member). In the second pulse the upthrown margin of the next fault block to the west was transgressed and deposition of basinal mudstones (Bernbjerg Formation) commenced in the basin centre on the main part of the dip-slope of the eastern block. Finally the crestal areas of the block on Kuhn Ø were inundated in Kimmeridgian times, and then subsided rapidly.