My current research at Vanderbilt University is under the Paleoecology concentration of Earth and Environmental Sciences. This research is overseen by Dr. Steve Goodbred Jr. and Dr. Neil Patrick Kelley with collaborators Dr. Simon Darroch and Dr. Michelle Casey. I am currently studying the origination, dispersal and paleo-environments of Mytilidae to explain modern biodiversity patterns and forecast how some species distributions will change to adjust to warming ocean waters. Please continue checking to see updates!
Present-day patterns of biodiversity are heavily influenced by processes operating on million-year timescales, including evolution, extinction, and tectonics. A fundamental unit of biogeography is geographic range, or the physical representation of the spatial area a species inhabits. By reconstructing historic geographic ranges of taxa through deep time, we can understand how various processes have influenced the modern abundance and distribution of species. Here, I use Mytilid (Family Mytilidae) bivalves – a clade with high preservation potential and an excellent fossil record – as a case study for reconstructing the historical biogeography of a clade in a phylogenetic context.
What are the modern biogeographic patterns of Mytilidae?
Where did the clade originate, and what are the characteristics of its ancestral range?
Preliminary results suggest that the ancestral mytilid was epifaunal, confined to the tropics, and possessed a large ancestral geographic range. Extant bivalve species disregard Rapoport’s rule as their biology effectively tethers them towards warmer temperatures – something that remains consistent when analyzing the ancestral state. With an expanded dataset incorporating both extant and fossil taxa, this work will help address longstanding questions in macroecology and macroevolution; specifically the role of biogeography in determining speciation and extinction risk, and to what extent different environmental perturbations (e.g., warming vs. cooling) produce differing effects on biogeographic patterns. Lastly, these data may help form the basis for a predictive ‘roadmap’ for how we expect species to respond to a variety of future global change scenarios.
Mytilidae are an extremely important clade of Bivalves whether you know it or not! You might've seen them anchored on wooden piers while you're swimming or sticking out of the peat on salt marshes. You might've come across them on your dinner plate at a restaurant or maybe you've seen their seashells washed up on the beach. Well, it turns out they have a very rich fossil record, dating back to around 425 million years ago to the end of the Silurian. Since Earth and its environments change over time, there must be a way to explain their modern distributions so we can better understand how their distributions will change in the future.
(Above) Paleogeographic map reconstructions through time. Red "+" indicate fossil occurences provided by Paleobiology Database (PaleobioDB.org)
Today, there are over 400 living species and over 50 genera of Mytilidae. A single mussel can filter up to 20 gallons of water and these mussels are found globally, inhabiting different environments and living different lifestyles that suit their needs.
(Right) Mapped geographic ranges of 31 taxa within Mytilidae. Pictures representing a taxa of each lifestyle (left to right), Lithophaga lithophaga (borer), Geukensia demissa (semi-infaunal), Musculus discors (infaunal) and Xenostrobus securis (epifaunal).
Occurrences of all Mytilid entries from GBIF
Relationship between species frequency (log-transformed) and latitude (absolute value) exemplifies Latitudinal Diversity Gradient.
Methods and Expertise
In this case, using latitudinal values from extant ranges reveal a possible tropical origin of ~28° N/S.
Using the fossil record can verify results produced from Phylogenetic models like Ancestor State Reconstruction.
(in press.)
Alejandro Prieto, Roman Zajac
Abstract -
Geukensia demissa (Atlantic Ribbed Mussel), a filter-feeding bivalve typically found in low marsh habitats spanning the Atlantic coast of North America, was examined across three southern Connecticut salt marshes to assess the extent to which it may be expanding its spatial distribution into high marsh habitats. The extent and pattern of high marsh occupation was related to the geomorphological and elevation characteristics of each marsh. Abundances of live mussels on the high marsh varied (1 to 46 individuals m-2) within and among marshes, and most were found in the lower and middle portions of the high marsh. Densities of dead mussels followed a similar pattern. Relatively large, live individuals were found across the high marsh, indicating Geukensia is able to grow in these habitats. The ratio of live to dead mussels varied among marshes, but at two sites was positive suggesting overall survivorship can maintain and increase their abundances on high marsh habitats. Relative to previous studies, Geukensia is increasing in high marsh habitats where tidal inundation is more frequent, likely as a consequence of sea level rise (SLR). Our results add to our understanding of the changing ecology of New England salt marshes in relation to SLR.
(Left) Schematic drawings of the (A) Pleasant Point, (B) Chaffinch Island and (C) Trolley Road salt marsh study sites showing the general low to upland marsh gradients in elevation and vegetation zones, and high marsh sections designated in this study. (Right) Approximate locations of transects at each site.
Small-scale variation in the abundance of live and dead Geukensia demissa in each quadrat along sampling transects at Pleasant Point and Chaffinch.