High concentration of long‐snouted beaked whales (genus Messapicetus) from the Miocene of Peru

Abstract: Eight skulls of beaked whales (Cetacea, Odontoceti, Ziphiidae), in six cases associated with elements of the mandible, were collected from a limited area (about 1.5 km²) and roughly from the same stratigraphic horizon at Cerro Colorado, 35 km south‐south‐west of the city of Ica (Peru), where the late Middle Miocene basal strata of the Pisco Formation crop out. They represent the highest concentration reported of fossil Ziphiidae. These finely preserved Cerro Colorado fossils are described and assigned to a new species Messapicetus gregarius, together with another specimen collected from sediments of the same age at Cerro la Bruja (33 km south‐east to Cerro Colorado). Messapicetus gregarius shares with M. longirostris Bianucci, Landini and Varola, 1992 (Tortonian of Italy), an extremely elongated rostrum, but is clearly different from the Italian species in the more distinct maxillary tubercle and prominential notch, the more robust premaxillary crest, and the abrupt ventrolateral descent of the medial margin of the maxilla from the vertex. A parsimony analysis reveals that Messapicetus belongs to a basal clade, which includes other ziphiids with a dorsally closed mesorostral groove and prenarial basin. The high concentration of specimens belonging to the same species (some of them tentatively identified as adult males and females), combined with the presence of a calf, supports the hypothesis of site fidelity; these cetaceans might have lived in a limited region for a long period for both breeding and feeding. Besides the eight specimens of M. gregarius, strata at Cerro Colorado include many other cetacean remains (with several specimens of the pontoporiid Brachydelphis including a foetus), pinnipeds, turtles, fishes, and birds.     

Soil respiration in a Mediterranean oak forest at different developmental stages after coppicing

To assess the variation of soil respiration at different forest stages we measured it in a coppiced oak (Quercus cerris L.) chronosequence in central Italy during two campaigns, spanning 2 successive years, in four stands at different stages of the rotation: 1 year (S1), 5 years (S5), 10 years (S10) and 17 years (S17) after coppicing. The contribution of the different components of soil respiration flux (aboveground litter, belowground decomposition soil organic matter and root respiration) was estimated by a paired comparison of manipulative experiments between the recently coppiced stand (S1) and mature stand (S17). Ninety percent of soil respiration values were between 1.7 and 7.8 μmol m^?2 s^?1, with an overall mean (±SD) of 4.0±2.7 μmol m^?2 s^?1. Spatial variation of soil respiration was high (CV=44.9%), with a mean range (i.e. patch size) of 4.8±2.7 m, as estimated from a semivariance analysis. In the absence of limitation by soil moisture, soil respiration was related to soil temperature with the exponential Q₁₀ model (average Q₁₀=2.25). During summer, soil moisture constrained soil respiration and masked its dependence on soil temperature. Soil respiration declined over the years after coppicing. Assuming a linear decline with stand age, we estimated a reduction of 24% over a 20‐year‐rotation cycle. The response of soil respiration to temperature also changed with age of the stands: the Q₁₀ was estimated to decrease from 2.90 in S1 to 2.42 in S17, suggesting that different components or processes may be involved at different developmental stages. The contribution of heterotrophic respiration to total soil respiration flux was relatively larger in the young S1 stand than in the mature S17 stand.     

Sero-systematic and taximetric studies on the Phaseoleae (Fabaceae) and related tribes

VIVIANI, T., CONTE, L., CRISTOFOLINI, G. & SPERANZA, M., 1991. Sero-systematic and taximetric studies on the Phaseoleae (Fabaceae) and related tribes. One hundred and fifty-two species of Phaseoleae, Desmodieae, Indigofereae, Millettieae, Sophoreae and Swartzieae were subjected to a taximetric study. The serological relationships were analysed using 37 antigenic systems and 12 antisera upon a representative sample from the six tribes. The comparative use of taximetric and serological data allowed the following conclusions to be drawn: (1) the tribe Phaseoleae is not a natural taxon; the primitive complex Diocleinae-Glycininae, the more derived Phaseolinae, and the Cajaninae deserve tribal rank; the position of the remaining subtribes requires further examination. (2) The Desmodieae are related to the Phaseoleae, whereas the Indigofereae have little relation to them. (3) The Baphia -group in the Sophoreae is possibly related to the Phaseoleae ancestors, while the other Sophoreae belong to different phyletic lines. (4) Swartzia is morphologically related to the Sophoreae, but does not belong to the same natural group. (5) Sophoreae, Millettieae and Phaseoleae are three heterogeneous aggregates representing stages of increasing specialization, rather than elements of a single phyletic line.