Comentarios biogeograficos y ecologicos sobre "A new neotropical species of the genus Parochlus Enderlein, 1912 (Chironomidae: Podonominae) and new distribution in Argentina" por Rodriguez et al. 2009.
Recently, Rodriguez et al. (2009) described a new species of the Podonominae genus Parochlus Enderlein. This genus has a wide distribution in the Andean Patagonian region with representatives in the Holarctic region and an undescribed species of the araucanus group in the higher elevations of Costa Rica. The new species Parochlus carollnae was fully described as adult male, pupa and larva. Very good drawings were provided showing the most important features of this species. However, several aspects of the abovementioned contribution concerning ecological and biogeographical aspects require some comments.
The new species was described based on an adult male collected with a sweep net and two pupae and three pupal exuviae (one of them with its larval exuvia attached) collected with a drift net. The type locality is Carolina stream, located in the hill system of North-Central San Luis Province (Argentina). The rest of the material was collected from the Grande River, also located in San Luis hills. The Carolina stream is a tributary of the Grande River and has an altitude of 1620 m a.s.l. at the type locality. Rodriguez et al. (2009) stated that the headwaters of this stream were located in La Carolina village, citing a paper of Tripole et al. (2000). In this paper, however, Tripole et al. (op.cit) established the origin for the Carolina stream in Tomolasta Hill, at 1969 m a.s.l.
Adult midges emerge at the water surface, irrespective of their submerged larval microhabitat, and the cast pupal case is left floating on the water surface. Several studies have shown that pupal exuviae can drift for approximately 200 to 400 m downstream and could remain on the water surface for about two days (e.g. Ruse, 1995) depending on several characteristics of the river such as, surface current velocity, substratum, discharge, turbidity, etc. Ruse (1995) sampled chironomid pupal exuviae and larvae from the same stretch of stream and compared their patterns of species assemblage. His results showed that pupal exuviae are good estimators of chironomid assemblages and that the greatest discrepancies between larval and pupal assemblages occurred with species recorded as pupal exuviae but absent as larvae. Marziali et al. (in press) highlighted the usefulness of pupal exuviae as a technique to evaluate chironomid richness, but these authors point out that although this technique facilitates species identification, it does not provide information of habitat preferences of the taxa. Rodriguez et al. (2009) mentioned that the new species was recorded at a mean temperature of 14.8 C. Based on this data, they extended the range of temperature for the genus. The immature stages of P carolinae were described from material collected with a drift net and therefore, it is not certain whether these materials were originated in the sampled area or upstream. In addition, several studies of chironomid larvae in the same river system (Tripole et al. 2000, Medina & Paggi, 2004; Medina et al., 2008) did not find any representatives of the subfamily Podonominae. For these reasons, the new temperature range proposed by Rodriguez et al. is only weakly supported by evidence and should be interpreted as tentative. New studies are needed to establish the actual ecological features of Parochlus carolinae, particularly focusing upstream and at the headwaters of the abovementioned localities.
The new species Parochlus carolinae is first record of the genus for Argentina outside the Andean-Patagonian domain. Rodriguez et al. (2009) stated that this new record occurred in the Monte biogeographic province, but neglected to mention the biogeographic scheme used as the basis for this statement. They also interpreted the presence of this species in San Luis Province as an Andean-Patagonian element in a biogeographic transition zone between the extensive arid lands to the South and the West (Patagonia, Monte, Puna) and the wetlands to the North and East of South America (Chaco). Rodriguez et al. based this statement on Morrone's (2004) assessment of the Monte biogeographic province as an ecotone between the Brazilian and Patagonian regions.
Following Cabrera & Willink (1973), the most cited biogeographic scheme for the Neotropics, San Luis hills is part of the Serrano district of the Chacoan province. Moreover, several biogeographical and ecoregional schemes (Bucher, 1980; Morrone, 2001; Olson et al., 2001) agree in considering the San Luis hills as part of or closely related to the Chacoan province. Curiously, Rodriguez et al. start the paragraph concerning the geographical distribution and ecology of Parochlus caroHnae by assigning the San Luis hills as part of the Chaco wetland. Based on their origin, Bucher & Chani (1998) classified the Chacoan wetlands into three major systems: a) wetlands formed by rivers and streams originated in the western mountain systems; b) wetlands formed by floods from the Parana and Paraguay rivers; and c) temporary shallow lakes and wetlands originated by local precipitations. It is important to point out that their classification made no mention of the rivers and streams belonging to the San Luis hills. The erroneous assignment of Parochlus carolinae as belonging to the Monte province by Rodriguez et al. (2009) rejects the biogeographic hypothesis proposed by those authors. The Monte province is a well-defined biogeographic unit, different from the Chacoan province (Roig-Junent et al., 2001). The presence of Parochlus carolinae in the Chacoan Serrano district has an important biogeographical significance. Frenguelli (1950) considered the San Luis hills as part of the peripampasic orogenic arc establishing a biotic corridor together with the hills in the Mahuidas, Tandilia and Ventania systems. A biotic migratory route from the Andes to Brazil, extending across the Pampean Mountain range, Buenos Aires hills, Uruguay hills, and Planalto and Brazilian hills, was postulated by several authors. Ringuelet (1961) detected a disjunctive distributional pattern supported by several taxa along the Pampean Mountain range, which has been corroborated by modern biogeographical analyses (Crisci et al., 2001; Roig-Junent et al., 2003 and literature cited in both papers). Roque & Trivinho-Strixino (2004) described the Podonominae species Podonomus pepinellii collected in Camanducaia (Brazil), located in the Serra da Mantiqueira, at an elevation of 1853 m asl. Tejerina & Molineri (2007) found podonomine larvae at high altitudes in the Pampean Mountain range. These records together with that of Parochlus carolinae suggest a possible biogeographic history similar to those described by Ringuelet (1961), Crisci et al. (2001) and Roig-Junent et al. (2003). In the Middle Miocene (ca. 11 Mya), southern South American landscapes began to be dominated by the uplift of the Andes. Thus, during this age the climate was cooler and with more marked seasonality than it had been in the early Middle Miocene. In the late Pliocene (ca. 3 Mya), a new Andean uplift resulted in the elevation of the Central Cordillera of Argentina and Chile and the eastern orographic systems of Argentina (Pampean Mountain range and Tandilia and Ventania systems among others). The final uplift of the Pampean Mountain range in central Argentina and the Central Andes of Chile had evident ecological consequences, since the areas situated between them acquired their current extremely xeric nature as a result of the rain shadow effect. During the Pleistocene (ca. 2.5 Mya), the planet underwent several glacial-interglacial cycles accompanied by the advance and retreat of continental glaciers. During the periods of glacial maxima, the climates of many non-glaciated temperate regions were cooler and dryer than those of today. Climatic changes associated with the glacial periods caused a general expansion of steppes, savannas, and open terrestrial ecosystems instead of close-canopied ecosystems such as tropical rain forests. The distributional pattern found in the Peripampasic orogenic arc, Uruguay hills and Planalto and Brazilian hills could be explained as a consequence of these events. In the case of cold- stenothermic taxa, such as the Podonominae, the progressive environmental cooling and the alternating periods of warm-wet and cold-dry conditions may have resulted in an eventual separation of populations and subsequent speciation, or may have favored the expansion of their distributional ranges and posterior isolation. These two possible hypotheses could be corroborated with future studies of the chironomid diversity in those areas.
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DONATO, Mariano and Paula POSADAS
Laboratorio de Sistematica y Biologia Evolutiva (LASBE), Museo de La Plata, Paseo del Bosque s/n (1900), La Plata, Argentina; e-mail: firstname.lastname@example.org; email@example.com
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|Title Annotation:||NOTA CIENTIFICA|
|Author:||Donato, Mariano; Posadas, Paula|
|Publication:||Revista de la Sociedad Entomologica Argentina|
|Date:||Jan 1, 2010|
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