Dominican Republic, part II

Hello there dear readers. Today I bring you the second installment of this series. Like I mentioned in the previous post we moved from the Albian to the Miocene.

The Miocene of the Dominican Republic is probably best known for the amber deposits. These have not only produced beautiful amber, which is used in jewelry, but also a number of fossil taxa have been described based on remains entombed in the amber. These fossils consist mostly of invertebrates, however, several vertebrates have been described as well, including anoles, frogs, and an insectivore. This gives us a glimpse into the smaller fauna that inhabited the island during the Miocene, in contrast to what is known from the same age in Puerto Rico and Cuba where most of the vertebrate fossils of that age consist of larger animals (sloths, rodents, primates, sirenians, crocodylians and turtles). A good summary of the vertebrates known from the Tertiary of the Greater Antilles can be found in table 1 of MacPhee et al. (2003) (free download here).

One of our first excursions into the Miocene was on a Wednesday afternoon. We spent the morning collecting the last samples from one of the outcrops of the Hatillo Limestone and some rudists from near the entrance of a cave in that same limestone unit. We then headed west towards the Monte Plata Province where we knew there was a new road cut exposing units of Miocene age.

The first outcrop of the Miocene that we visited. This is actually one of the best Miocene outcrops I've seen in a while.

By the time we got there it was near the middle of the afternoon, which meant we didn’t had much sunlight left. We stopped in the first large outcrop we saw (Picture above) and it was worth it! We quickly started finding turtle shell fragments, and occasionally we saw cross sections of turtle shells that went into the outcrop. I decided to collect one of these. It was not big, and as I found out after prep work, not too good (see pictures below). However, it was worth going there, as there is more material to be found and collected!

Top left: me overturning the jacket with the turtle shell remains; top right: the jacket back in the lab; bottom left: view of the jacket when it was first opened; bottom right: the fossil turtle remains. (Click on the image to see the larger version.)

Several days latter we had some free time, so we decided to go back to this area. This time we drove in from the north, driving through Los Haitises where we saw beautiful karst topography. Our time was limited in this occasion as well, but we made the most out of it.

The second outcrop we visited, smaller than the first one, but still interesting. Alvin Bonilla for scale.

We hit a couple of outcrops (Picture above) where we found the usual (at least what usual for the Tertiary of Puerto Rico and Cuba); croc teeth, turtle shells and sirenians (which was what I was really after). The sirenian material was in a concretion, half of it which had fallen off the outcrop so it made it easy to collect. The other part is still in the outcrop and I hope to go back sometime in the spring to collect it. Actually, if it wasn't for Alvin, who saw it, I almost stepped on the part that had fallen trying to get a better view of the part still in the outcrop. After some prep work on the sirenian material it turned out to be mostly ribs, and a few vertebrae. However, even if it is a little frustrating, it will nonetheless be an important contribution to the understating of sirenian distribution during the Miocene of the Caribbean and demonstrates that there is probably more, better material waiting to be collected!

Top left: me collecting the concretion with the sirenian remains; top right: view of the jacket in the lab; bottom left: the jacket, recently opened; bottom right: the concretion, as of now, still need some prep work to be done. Oysters (near the center of the concretion and to the right) used some of the ribs as hardground. (Click on the image to see the larger version.)

MacPhee, R. D. E., M. A. Iturralde-Vinent & E. S. Gaffney. 2003. Domo de Zaza, an Early Miocene vertebrate locality in south-central Cuba, with notes on the tectonic evolution of Puerto Rico and the Mona Passage. American Museum Novitates 3394:1-42.

Fossil side-necked turtles from Puerto Rico

As I have learned through my many fieldtrips around Puerto Rico one of the most common fossils in the Cenozoic rocks are fragments of turtle shells. In fact one of the first vertebrate fossils I collected (back in 2001) was a turtle shell from the Juana Díaz Formation (early Oligocene, ~31 million years ago), which was for a while on exhibit in the now defunct Geology Museum at the Department of Geology, University of Puerto Rico, Mayagüez Campus. As I latter found out, this fossil represented a shell of a pelomedusoid turtle, more commonly known as side-necked turtles. Nonetheless it wasn’t the first time that fossil side-necks or other kinds of turtles were found as fossils in Puerto Rico.

Representatives of side-necked turtles; two Podocnemis, possibly, P. unifilis, photo taken in Guayaquil, Ecuador in 2018.

One of the first accounts about fossil turtles from Puerto Rico is found in Rabell-Cabrero (1914) where he briefly mentions the occurrence of turtle costal and neural plates among other vertebrate remains that he had collected. This material was collected around Salto Collazo in the town of San Sebastián (northwestern PR), which means that the fossils came from Oligocene age rocks (Rabell-Cabrero, 1914; MacPhee and Wyss, 1990). Most of the vertebrate material collected by Rabell-Cabrero was later donated to the American Museum of Natural History (MacPhee and Wyss, 1990), while a small portion remained in the Museo de Zoología at UPR-RP (or at least there was when I visited in 2007).

Eventually, some of the specimens collected by Rabell-Cabrero was studied and described by Roger C. Wood and published in 1972. In his paper, Wood describes a shell, plastron and pelvis collected from the San Sebastian Formation (early-late Oligocene age) but due to the incompleteness of the material no species name was given, although similarities with living and extinct South American pelomedusids were noted (Wood, 1972).

Photos from one of my research sites in Puerto Rico, the red circles mark parts of a pelomedusoid turtle shell, the green circle, a sirenian rib. I wrote about this locality here.

Additional fossils of side-necked turtles were discovered in Puerto Rico during the late 1980’s American Museum of Natural History expeditions. These came from early to middle Miocene deposits in northern PR and included a shell, proximal humerus and pubis (MacPhee and Wyss, 1990). Although, as they mention, the material is well preserved, a proper description is still pending. This might be in part because the conservative shell morphology of most pelomedusoids makes identification below family level difficult (Gaffney and Zangerl, 1968; Wood and Diaz de Gamero, 1971; MacPhee et al. 2003).

Skull of Bairdemys hartsteini, photos from Gaffney and Wood, 2002. 

In the early 2000's a pelomedusoid skull from Puerto Rico was described by Gaffney and Wood (2002). This skull (see photos above) is the type species of Bairdemys harsteini, a new genus that also includes several species from around the Americas, including B. venezuelensis (formerly known as Podocnemis venezuelensis; Wood and Diaz de Gamero, 1971), B. sanchezi, B. winklerae, B. healeyorum, and B. thalassica (Gaffney and Wood, 2002; Gaffney et al. 2008; Weems and Knight, 2013; Ferreira et al., 2015). Bairdemys harsteini was collected from the early-middle Miocene deposits of the Cibao Formation in northern Puerto Rico, in addition to the skull, some shell fragments collected by MacPhee and Wyss (1990) from a nearby locality has been referred to this taxon (MacPhee et al. 2003). One interesting aspect of the Venezuelan species, B. venezuelensis, is that the shells do not have neural bones in the carapace, which might be an autapomorphy of that taxon (the carapace of the other species is still unknown), as neurals seem to be present in the shell material assigned to B. harsteini (Wood and Diaz de Gamero, 1971; Gaffney and Wood, 2002; Gaffney et al., 2008). 

Now going back to the Juana Díaz pelomedusoid I mentioned at the beginning. This shell, although missing about the anterior half, does have at least three neural plates, and seems to have been approximately the same size as the material described by Wood (1972), which also has neural plates. Unfortunately, no additional material from the Juana Díaz Formation has been collected recently, so the precise identity of that turtle is still unknown. Other turtle material I have been collecting over the last 15 years primarily comes from the San Sebastian Formation and Lares Limestone (early-late Oligocene age-northern PR). So far all that material seems to be from side-necks and is fairly similar in size and morphology to the Juana Diaz carapace and the San Sebastian form of Wood (1972) (see drawing comparing these with a Cuban shell mentioned below).

A few other fossil side-necks are known from the Greater Antilles, such as Caribemys oxfordiensis from the Jurassic of Cuba, and an unknown pelomedusoid from the early Miocene of Cuba (de la Fuente and Iturralde-Vinent, 2001; MacPhee et al., 2003). Nevertheless, there is still a lot of work, particularly with the fossils from Puerto Rico as I'm pretty sure there is more than one new species waiting to be discovered/described. This particular groups of turtles is nowadays absent in Puerto Rico, at least naturally, so these fossils, like many others, allow us to get a glimpse into the ancient fauna of the island and understand how it has change throughout its geologic history.

References

de la Fuente, M. S., and M. A. Iturralde-Vinent. 2001. A new pleurodiran turtle from the Jagua Formation (Oxfordian) of western Cuba. Journal of Paleontology 75:860-869.

Ferreira, G. S., A. D. Rincón, A. Solórzano, and M. C. Langer. 2015. The last marine pelomedusoids (Testudines: Pleurodira): a new species of Bairdemys and the paleoecology of Stereogenyina. PeerJ 3:e1063.

Gaffney, E. S., and R. C. Wood. 2002. Bairdemys, a new side-necked turtle (Pelomedusoides: Podocnemididae) from the Miocene of the Caribbean. American Museum Novitates 3359:1-28.

Gaffney, E. S., and R. Zangerl. 1968. A revision of the chelonian genus Bothremys (Pleurodira: Pelomedusidae). Fieldiana Geology 16:193-239.

Gaffney, E. S. T. M. Scheyer, K. G. Johnson, J. Bocquentin, and O. A. Aguilera. 2008. Two new species of the side necked turtle genus, Bairdemys (Pleurodira, Podocnemididae), from the Miocene of Venezuela. Paläontologische Zeitschrift 82(2):209-229.

MacPhee, R. D. E. and A. R. Wyss. 1990. Oligo-Miocene vertebrates from Puerto Rico, with a catalog of localities. American Museum Novitates 2965:1-45.

MacPhee, R. D. E., M. A. Iturralde-Vinent, and  E. S. Gaffney. 2003. Domo de Zaza, an Early Miocene vertebrate locality in south-central Cuba, with notes on the tectonic evolution of Puerto Rico and the Mona Passage. American Museum Novitates 3394:1-42.

Rabell-Cabrero, N. 1914. Notas paleontológicas. Revista de las Antillas 2(1):66-69.

Weems, R. W., and J. L. Knight. 2013. A new species of Bairdemys (Pelomedusoides: Podocnemididae) from the Oligocene (early Chattian) Chandler Bridge Formation of South Carolina, USA, and its paleobiogeofraphic implications for the genus. In: Brinkman, D., P. Holroyd, J. Gardner (eds), Morphology and evolution of turtles, Vertebrate Paleoanthropology series. Netherlands: Dordrecht, 289-303.

Wood, R. C. 1972. A fossil pelomedusid turtle from Puerto Rico. Breviora 392:1-13.

Wood, R. C., and M. L. Diaz de Gamero. 1971. Podocnemis venezuelensis, a new fossil pelomedusid (Testudines, Pleurodira) from the Pliocene of Venezuela and a review of the history of Podocnemis in South America. Breviora 376:1-23.

Updated: May 23, 2019