The sibling polychaetes Platynereis dumerilii and Platynereis massiliensis in the Mediterranean Sea: are phylogeographic patterns related to exposure to ocean acidification?

2017 ◽  
Vol 164 (10) ◽  
Author(s):  
Janine Wäge ◽  
Giulia Valvassori ◽  
Jörg D. Hardege ◽  
Anja Schulze ◽  
Maria Cristina Gambi
2015 ◽  
Vol 5 (1) ◽  
Author(s):  
Susana Flecha ◽  
Fiz F. Pérez ◽  
Jesús García-Lafuente ◽  
Simone Sammartino ◽  
Aida. F. Ríos ◽  
...  

2017 ◽  
Vol 186 ◽  
pp. 125-138 ◽  
Author(s):  
Mauro Celussi ◽  
Francesca Malfatti ◽  
Franzo Annalisa ◽  
Frédéric Gazeau ◽  
Antonia Giannakourou ◽  
...  

2018 ◽  
Vol 190-191 ◽  
pp. 20-30 ◽  
Author(s):  
Narimane Dorey ◽  
Sophie Martin ◽  
François Oberhänsli ◽  
Jean-Louis Teyssié ◽  
Ross Jeffree ◽  
...  

2021 ◽  
Vol 4 ◽  
Author(s):  
Marcos A. L. Teixeira ◽  
Arne Nygren ◽  
Ascensão Ravara ◽  
Pedro E. Vieira ◽  
José Carlos Hernández ◽  
...  

Recent studies reporting complexes of cryptic or pseudo-cryptic species with narrow geographic distributions have been challenging the cosmopolitan status of a fair number of marine benthic invertebrates. Morphologically similar species are often overlooked but molecular techniques have been extremely effective in signalling potential hidden diversity which, complemented with further detailed examination, might reveal unique morphological and ecological features. Evidence of morphological stasis, where no clear and stable morphological differences are apparent, can be exemplified by the annelids Platynereis dumerilii (Audouin & Milne Edwards, 1833) and Platynereis massiliensis (Moquin-Tandon, 1869). These sibling species, usually found among algae in marine intertidal and subtidal habitats, can only be distinguished by their different reproductive strategies and life histories. The former is gonochoric, with a single reproductive event in life (semelparous) transforming into a pelagic epitokous form called heteronereis, has free spawning synchronized by lunar periodicity and a larval stage with planktotrophic development; while the latter shows no epitokous transformation and is a protandrous hermaphrodite, characterized by egg brooding and lecithotrophic larval stages with a semi-direct development. In order to verify the possible existence of additional hidden Platynereis species within the P. dumerilii morphotype, we used a multi-locus approach to investigate 26 populations along Europe from the NE Atlantic and the Macaronesia islands (Azores, Madeira and Canaries) to the Western and Eastern Mediterranean Sea. We concatenated the mtDNA COI-5P, rDNA 16S and 28S-D2 sequences and performed a phylogenetic analysis through Bayesian inference (BI). To depict Molecular Operational Taxonomic Units (MOTUs), we applied three delimitation methods (ABGD, bPTP and GYMC) to the concatenated alignment, except for COI where we also applied the Barcode Index Number (BIN), implemented in BOLD, which is exclusive to this locus. Consensus MOTUs were defined based on the majority rule and, in case of draw, the most conservative MOTUs were chosen. We detected at least 14 MOTUs with 23.1% COI mean K2P distance (6.6 - 32.6%). The BI tree is split into three major clades (Clade A: MOTUs 1-3, Clade B: MOTUs 4-9 and Clade C: MOTUs 10-14), with MOTU 3 appearing to represent P. dumerilii sensu stricto and MOTU 9 P. massiliensis. This assumption is based on data from the Type locality and a previous study by Wage et al. (2017), which combined phylogeographic (COI barcode region), reproductive biology and life-history observations on some selected Platynereis populations thriving in the vent areas from the Italian islands of Ischia and Vulcano. Major Cade C seems to be pseudo-cryptic as some visible differences can be found in the specimens, as for example, the size of the tentacular cirri and lack of dorsal pigmentation, in contrast with Clades A and B, where only differences in pigmentation types were found so far. The Spanish archipelago of the Canary Islands and the whole Mediterranean Sea seem to be a cryptic hotspot. Five MOTUs are unique to the Macaronesia and five sympatric MOTUs are present in the Gran Canaria and La Palma islands alone. Additionally, three lineages were present exclusively in the Mediterranean with four sympatric MOTUs spotted in the southeast of Spain (Calpe) and the Greek island of Crete. Three out of four NE Atlantic MOTUs are shared with the Mediterranean with one exclusive to this part of the continent. Failure to recognise this hidden biodiversity may compromise the accuracy and the interpretation of biomonitoring data or other relevant ecological studies. Integrative taxonomy is thus essential to solve these uncertainties and to allow naming the involved undescribed species. Otherwise, most molecular data providing enough support for species hypothesis will continue to be unused, and large fractions of biodiversity will persist unnoticed.


2022 ◽  
Vol 8 ◽  
Author(s):  
Cosimo Solidoro ◽  
Gianpiero Cossarini ◽  
Paolo Lazzari ◽  
Giovanni Galli ◽  
Giorgio Bolzon ◽  
...  

We simulate and analyze the effects of a high CO2 emission scenario on the Mediterranean Sea biogeochemical state at the end of the XXI century, with a focus on carbon cycling, budgets and fluxes, within and between the Mediterranean sub-basins, and on ocean acidification. As a result of the overall warming of surface water and exchanges at the boundaries, the model results project an increment in both the plankton primary production and the system total respiration. However, productivity increases less than respiration, so these changes yield to a decreament in the concentrations of total living carbon, chlorophyll, particulate organic carbon and oxygen in the epipelagic layer, and to an increment in the DIC pool all over the basin. In terms of mass budgets, the large increment in the dissolution of atmospheric CO2 results in an increment of most carbon fluxes, including the horizontal exchanges between eastern and western sub-basins, in a reduction of the organic carbon component, and in an increament of the inorganic one. The eastern sub-basin accumulates more than 85% of the absorbed atmospheric CO2. A clear ocean acidification signal is observed all over the basin, quantitatively similar to those projected in most oceans, and well detectable also down to the mesopelagic and bathypelagic layers.


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