Detection of the elusive Dwarf sperm whale (Kogia sima) using environmental DNA at Malpelo island (Eastern Pacific,Colombia)

1. Monitoring large marine mammals is challenging due to their low abundances in general, an ability to move over large distances and wide geographical range sizes.
2. The distribution of the pygmy (Kogia breviceps) and dwarf (Kogia sima) sperm whales is informed by relatively rare sightings, which does not permit accurate estimates of their distribution ranges. Hence, their conservation status has long remained Data Deficient (DD) in the Red list of the International Union for Conservation of Nature (IUCN), which prevent appropriate conservation measures.
3. Environmental DNA (eDNA) metabarcoding uses DNA traces left by organisms in their environments to detect the presence of targeted taxon, and is here proved to be useful to increase our knowledge on the distribution of rare but emblematic megafauna.
4. Retrieving eDNA from filtered surface water provides the first detection of the Dwarf sperm whale (Kogia sima) around the remote Malpelo island (Colombia).
5. Environmental DNA collected during oceanic missions can generate better knowledge on rare but emblematic animals even in regions that are generally well sampled for other taxa.

     

Postnatal Development and Possible Ligand Function of the CNS-Specific Membrane Glycoprotein CNSgp 130

CNSgp 130 is a CNS-specific membrane glycoprotein present in large amounts in the adult mammalian CNS. Using immunohistological techniques, we demonstrated that CNSgp130 is not detectable in the rat cerebellum at birth, and does not appear in the cerebellum until the tenth day of postnatal life. It is expressed first in the white matter of the cerebellar folia, and subsequently (by day 14) it is expressed also in the molecular layer. Expression in the granular layer is not seen until the 18th day of postnatal life, by which time the adult pattern of expression is established. CNSgp130 is also not detectable in the cerebrum at birth. However, it is expressed weakly but diffusely in the cerebrum by the fourth day of life. By the 10th day, there is strong expression in the cerebrum, in marked contrast to its virtual absence from the cerebellum at this stage. By quantitative absorption analysis, CNSgp 130 was undetectable on the day of birth, and increased steadily to 80% of adult values by the 22nd day of postnatal life. Binding studies with pure CNSgp130 demonstrated a Pronase-sensitive ligand in adult chicken brain. This ligand was absent from neonatal rat brain and non-CNS tissues.     

Nitrogen cycling in two riparian forest soils under different geomorphic conditions

At the floodplain scale, spatial pattern and successional development of riparian vegetation are under the control of geomorphic processes. The geomorphic and hydraulic characteristics of stream channels affect the sorting of organic material and inorganic sediment through erosion/sedimentation during floods. In turn, the proportion of fine sediments fractions differs by location within a given community of riparian forest succession. In this paper we tested the effect of geomorphic features of floodplains, through soil grain size sorting, on the nitrogen cycling in riparian forest soils. Two typical riparian forests formed by vertical accretion deposits from repeated addition of sediments from overbank flow have been chosen along the River Garonne, southwest France. These riparian forests had equivalent vegetation, flood frequency and duration, differing only in soil grain size composition: one riparian forest had sandy soils and the other had loamy soils. The evolution of the main soil physical and chemical parameters as well as denitrification (DNT), N uptake (N _U ) and mineralization (N _M ) rates were measured monthly over a period of 13 months in the two study sites. The loamy riparian forest presented a better physical retention of suspended matter during floods. Moreover,in situ denitrification rates (DNT) and N uptake by plants (N _U ) measured in the loamy riparian forest soils were significantly greater than in the sandy soils. Although DNT and N _U could be in competition for available nitrogen, the peak rates of these two processes did not occur at the same period of the year, N _U being more important during the dry season when DNT was minimum, while DNT rates were maximum following the spring floods. N retention by uptake (N _U ) and loss by DNT represented together the equivalent of 32% of total organic nitrogen deposited during floods on the sandy riparian forest soils and 70% on the loamy ones. These significant differences between the two sites show that, at the landscape level, one should not estimate the rates of N _U and DNT, in riparian forests soils only on the basis of vegetation, but should take also into account the geomorphic features of the floodplain.