How Eurypterids of the Finger Lakes, New York Lived and Died

Paleoecology and Taphonomy of Some Eurypterid-bearing Horizons in the Finger Lakes Region of New York State

Stephen M. Mayer

This news article was summarized by Alexander Favaro. Alexander Favaro is a first-generation student attending the University of South Florida, pursuing a B.S. in Geology. He hopes to follow his passion of being a paleobiologist. His interests have been broadly focused on paleoecology and understanding evolutionary trends. 

What data were used? The study used well-preserved fossils from the upper Silurian Fiddlers Green Formation in New York, the Lower Devonian Olney Member in Finger Lakes New York, Split Rock Quarry near Syracuse New York, and the Samuel J. Ciurca Eurypterid Collection at Yale Peabody Museum of Natural History. These data were used to make interpretations of eurypterid lifestyles and processes of fossilization. 

Methods: Sedimentological variables and the body and trace fossils found within a rock unit were used to interpret the depositional environment (what type of environment the rocks were formed in) of a formation. Field collection was done at the Phelps Member and Cayuga Junction (which are located in the Fiddlers Green Formation), as well as Split Rock Quarry in Syracuse, New York. The Yale Peabody Museum of Natural History was used to supplement eurypterid data through their collection. The position in which each eurypterid was found, as well as their size, was used to describe their age, ecology, and how they likely died.

Figure 1. Eurypterus remipes, which shows the U-shaped body posture. The metasoma (last 7-12 segments of the eurypterid) and telson (spine like protrusion at the end of the abdomen on the right of this image) were twisted 1260 in relation to the prosoma (head section) and mesosoma (first 1-6 segments of the eurypterid). This specimen was found in the Phelps Member, New York.

Results: Many eurypterid exuviae (shed exoskeleton) were found, while eurypterid bodies were less abundant. The most common eurypterid fossils found in Phelps were Eurypterus remipes. Cayuga Junction also possessed Eurypterus remipes but were far less common. At Split Rock Quarry, Erieopterus microphthalmus were found in localized calcareous (chalky limestone) bands. 

 The study found that between 61 carapaces, the average size of eurypterids in the Phelps Member fell between 15-25mm. The variations in size indicated that immature species and adults were living amongst each other. 

Since eurypterids were chelicerate arthropods (like arachnids, sea spiders, and horseshoe crabs), scientists have suggested that eurypterids would undergo a group spawning and then molt (shed their exoskeleton) together (similarly to a horseshoe crab). This would explain the high number of shed exuviae and variable size ranges found in the formations.

Fossil evidence indicated that eurypterid corpses were highly affected by currents, which would cause a variety of contortions in a carcass. The observed eurypterid corpse conditions were categorized as: a non-contorted corpse, an angular contortion up to 900, a U-shaped flexure of the body and tail (as seen in Figure 1), and a contortion where the body and tail flipped above or below the head (though this was rare). Aside from flexure of the body, some contortions were caused by sediment that anchored a section of the eurypterid while the un-covered portions moved freely due to current movement. Eurypterus remipes and Erieopterus microphthalmus both displayed similar contortions and so they were able to determine that the contortion patterns weren’t exclusive to one genus of eurypterid. 

Why is this study important? The study gave insight into the life and death of a once thriving taxon that has close relatives still alive today in the form of arachnids, sea spiders, and horseshoe crabs. Fossil evidence at Phelps suggested that eurypterids may have mass-molted, similarly to horseshoe crabs. The paleoecological evidence found gave a key insight into a behavior which has also been observed in modern, related organisms.

The big picture: The analysis performed on both trace fossils and carcasses gave both paleoecological and taphonomic (how an organism is fossilized after death) insight. Combined, taphonomy and paleoecology provides a more refined idea of how ancient organisms lived, died, and how their bodies would have been fossilized. 

Citation: Mayer, S. M. Paleoecology and Taphonomy of Some Eurypterid-Bearing Horizons in the Finger Lakes Region of New York State.

How Climate Change in Serbia is Impacting the Rate of Cancer and Infectious Diseases

Assessment of climate change impact on the malaria vector Anopheles hyrcanus, West Nile disease, and incidence of melanoma in the Vojvodina Province (Serbia) using data from a regional climate model 

By: Dragutin T. Mihailović, Dusan Petrić, Tamas Petrović, Ivana Hrnjaković- Cvjetković, Vladimir Djurdjevic, Emilija Nikolić-Đoric, Ilija Arsenić, Mina PetrićID, Gordan Mimić, Aleksandra Ignjatović-Cupina 

Summarized by: Kailey McCain

What data were used? Researchers assessed climate change and UV radiation (UVR) and compared it to data collected over ten years from mosquito field collections at over 166 sites across Serbia. Additionally, public health records for the circulation of vector-borne disease (I.e., illnesses spread by mosquitoes and ticks), specifically the West Nile Virus, and the incidence of melanoma (i.e., a serious form of skin cancer) were collected and compared.

Methods: The climate change and UVR doses were collected by using EBU-POM model (a type of regional climate model) for the time periods: 1961-2000 and 2001-2030. As for the collection of the mosquito data, two different dry-ice baited traps (dry-ice is a solid form of carbon dioxide, which is a natural attractive substance for mosquitos) were used. The various sites were chosen by entomologists (i.e., scientists who study insects) to obtain a diverse data set. The mosquitoes collected were then anesthetised, separated by location, species, sex, and then tested for a specific RNA (I.e., a single stranded molecule) strand that would indicate the mosquito was carrying the West Nile Virus.

Furthermore, the researchers measured the rate of melanoma incidences in Serbia by using two different indicators: new number of cases versus time and number of new cases versus population size. The defined time period for data collection was 10 years (1995-2004). With this data, the researchers compared the rate of incidence to the climate data previously collected.

Fig 1: This diagram shows the linear trend in annual temperature fluctuations throughout Serbia from the time period 1990-2030; as well as depicts the mosquito prevalence found at the various collection sites.

Results: From the data collected via the regional climate model, a linear upwards trend in temperature in Serbia was recorded. The prevalence of mosquitoes was also found to increase linearly throughout the time period. The culmination of these results can be seen in figure 1.

As for the melanoma data, the researchers found a linear increase in UVR doses for the time period. This data was found to be correlated to an increase in melanoma incidences throughout Serbia and this data can be visualized in figure 2.

Why is this study important? Disease prevalence and distribution have always been difficult to predict due to the varying ecological factors that play important roles. Research like this is especially important because it allows scientists to simulate future spreads of vector-borne diseases within European countries. This can eventually lead to the development of public health surveillance technology and overall prevention.

Fig 2: Diagram (a) depicts the increased temperature rates throughout Serbia, and diagram (b) depicts the UV radiation doses on the various provinces throughout Serbia. Diagram (c) shows the linear relationship of UV doses versus the time period 1990-2030. The data shows a clear increase in “hot days” (HD) and “warm days” (WD) through time. Diagram (d) shows a linear relationship between UVR dose versus melanoma incidence rate from 1995-2004.

The big picture: This study aimed to correlate changes in temperature and UV radiation to the spread of diseases and cancer. With vector-borne diseases being the most sensitive to ecological conditions, researchers chose the West Nile Virus to act as a proxy to all mosquito transmitted diseases. As expected, the data supports the claim that increased temperatures trigger an enhanced risk for not only infectious diseases, but certain cancers as well.

Citation: Mihailović, D. T., Petrić, D., Petrović, T., Hrnjaković-Cvjetković, I., Djurdjevic, V., Nikolić-Đorić, E., Arsenić, I., Petrić, M., Mimić, G., & Ignjatović-Ćupina, A. (2020). Assessment of climate change impact on the malaria vector Anopheles hyrcanus, West Nile disease, and incidence of melanoma in the Vojvodina Province (Serbia) using data from a regional climate model. PLoS ONE, 15(1), 1–17. https://doi.org/10.1371/journal.pone.0227679

How coastal wetlands can help reduce property damage from storm surge and sea level rise

Valuing natural habitats for enhancing coastal resilience: Wetlands reduce property damage from storm surge and sea level rise

by: Ali Mohammad Rezaie, Jarrod Loerzel, Celso M. Ferreira

Summarized by: Mckenna Dyjak

What data were used?: This study used coastal storm surge modeling and an economic analysis to estimate the monetary value of wetland ecosystem services (positive benefits of natural communities to people). One of the ecosystem services provided by wetlands is that  they are great at controlling flooding; their flood protection value was estimated using the protected coastal wetlands and marshes near the Jacques Cousteau National Estuarine Research Reserve (JCNERR) in New Jersey. 

Methods: Storm surge flooding was determined for historical storms (e.g., Hurricane Sandy in 2012) and future storms that account for habitat migration and sea level rise. Each storm had modelled flooding scenarios for both the presence and absence of the coastal wetland/marsh. The model also incorporated ways to account for monetary value of physical damage by using property values.

Results:  This study found that coastal wetlands and marshes can reduce flood depth/damage by 14% which can save up to $13.1 to $32.1 million in property damage costs. The results suggest that one square kilometer (~0.4 square miles) of natural coastal wetland habitats have a flood protection value of $7,000 to $138,000 under future conditions (Figure 1).

Figure 1. This graph shows the estimated monetary value of coastal marshes flood protection in different storm scenarios per square kilometer. A “25 year Storm” or “50 year Storm” is a storm event that occurs once on average in the time span given.

Why is this study important?: Natural coastal wetlands and marshes contribute many vital ecosystem services such as providing habitats for wildlife, helping protect against coastal erosion, and purifying water. Assigning a monetary value to these natural habitats for their flood protection can highlight another aspect of their importance and urge people to protect these important coastal communities. The results from this study can allow the public and private sectors to develop and practice sustainable methods to preserve the ecosystems.

The bigger picture: Storm events, such as hurricanes, are predicted to become more frequent and more severe due to climate change. As the oceans continue to warm (an estimated increase of 1-4 degrees Celsius in mean global temperatures by 2100) hurricanes are predicted to intensify in wind speed and precipitation. Storm surge is known to be the most dangerous aspect of hurricanes and causes deadly flooding. As sea levels rise and ocean water expands due to warming, storm surges will become more severe during major storm events. This study has shown that coastal wetlands and marshes are considered our “first line of defense” in these circumstances. We must take care of and protect our natural habitats because they provide us with many services that we are unaware and likely unappreciative of.

Citation: Rezaie AM, Loerzel J, Ferreira CM (2020) Valuing natural habitats for enhancing coastal resilience: Wetlands reduce property damage from storm surge and sea level rise. 

How fossil collection methods can affect paleoecological datasets

The influence of collection method on paleoecological datasets: In-place versus surface-collected fossil samples in the Pennsylvanian Finis Shale, Texas, USA

Frank L. Forcino, Emily S. Stafford

Summarized by Mckenna Dyjak

What data were used?: Two different fossil collecting methods were compared using the Pennsylvanian marine invertebrate assemblages of the Finis Shale in Texas. In-place bulk-sediment methods and surface sampling methods were used to see how these different methods could influence taxonomic (groups of animals) samples. 

Methods: The bulk-sediment sampling method involves removing a mass of sediment and later washing and sieving the material to retrieve the fossil samples; surface sampling is a simpler method in which the top layer of sediment is removed and the exposed fossils are collected by hand. The samples were collected in the Finis Shale in Texas at stratigraphically equivalent (layers of rock deposited at the same time) locations to ensure continuity in the two methods. The bulk-sediment and surface pick-up samples were analyzed for differences in composition and abundance of fossil species (i.e., paleocommunities) using PERMANOVA (a type of analysis used to test if samples differ significantly from each other).

Results: The study found that the bulk-collected samples differed from the surface-collected samples. The relative abundance of the major taxonomic groups (brachiopods and mollusks), composition, and distribution varied considerably in both collecting methods. For example, there was a higher relative abundance of brachiopods in the bulk-collected samples and a higher relative abundance of gastropods in the surface-collected samples.

Figure 1. Comparison of relative abundance of fossil groups between in-place and surface samples. Note the different abundances from each of the collection methods.
(SpE = Spillway East outcrop, SpW = Spillway West outcrop, CW = Causeway Road outcrop)

Why is this study important?: Bulk-sediment sampling and surface sampling methods produce significantly different results, which would end up affecting the overall interpretation of the history of the site. The surface-collected fossils may be influenced by stratigraphic mixing (mixing of materials from different rock layers), collector bias (which can influence a fossil’s potential to be found and collected; for example, larger fossils are more likely to be collected), and destruction of fossils due to weathering. Bulk-sediment sampling will likely have a more accurate representation of the ancient community, because the fossils likely experienced the least amount of alteration during the process of the organism becoming a fossil (also known as taphonomy).

The bigger picture: The amount of things that have to go right in order for an organism to become a fossil is a lengthy list (read more about the fossilization process here). There are many biases that can contribute to the incompleteness of the fossil record such as environments that favor preservation (e.g., low oxygen), as well as poor preservation value of soft tissues, like skin. Scientists must do what they can in order to collect accurate data of the fossil record since there are already so many natural biases. Knowing which fossil collecting methods produce the most accurate results is important when advocating for the paleocommunity.

Citation: Forcino FL, Stafford ES (2020) The influence of collection method on paleoecological datasets: In-place versus surface-collected fossil samples in the Pennsylvanian Finis Shale, Texas, USA. PLoS ONE 15(2): e0228944. https://doi.org/10.1371/journal.pone.0228944

Organic carbon stored in Florida lakes

Organic carbon sequestration in sediments of subtropical Florida lakes

Matthew N. Waters, William F. Kenney, Mark Brenner, Benjamin C. Webster

Summarized by Mckenna Dyjak

What data were used? A broad range of Florida lakes were chosen based on size, nutrient concentrations (nitrogen and phosphorus), trophic state (amount of biologic activity that takes place), and location. The lakes were surveyed using soft sediment samples to identify the best drilling sites for sediment cores. After drilling, the cores were dated and the organic carbon (OC) content and burial rates were calculated. Organic carbon can be stored in sediments and buried, which temporarily removes it from the atmosphere.

Methods: The sediment cores were taken using a piston corer commonly used to retrieve soft sediments. Each core was dated using ²¹⁰Pb which is a common radioactive isotope found in lake environments and can be used to date sediments up to 100 years. Radioactive isotopes can be used to date rocks and sediments based on their natural decay rate (half-life). The organic carbon content of the cores was measured using a Carlo-Erba NA-1500 Elemental Analyzer which is an instrument that can determine the total carbon present in a sediment sample. To calculate the organic carbon deposition rates, the accumulation of sediment rates were multiplied by the proportion of OC found in the sediment. A recent increase of eutrophication (high amount of nutrients present in lakes) needed to be taken into account when calculating the OC deposition rate, so the sediments were divided into pre-1950 and post-1950 deposits to depict the change in industrial activity and agriculture. 

Results: The OC burial rate was highest in the shallower lakes and decreased as the depths increased (can be seen in Figure 1). This is different from the rates for temperate (mild temperatures) bodies of water, where OC burial rates decreased as the lakes got bigger. They found a 51% increase in OC burial rates in the post-1950 deposits which corresponds to the increase in eutrophication in the lakes.

Figure 1. Graph showing the correlation between depth and organic carbon (OC) burial rate. The OC burial rate increases as the depth decreases in meters.

Why is this study important? Cultural eutrophication is caused by an increase of nutrients in waterways such as phosphorus and nitrogen (commonly found in lawn fertilizers) which cause harmful algal blooms; these algal blooms remove oxygen from the water and can mess up the entire ecosystem. The lack of oxygen and harmful algal blooms can lead to habitat loss and loss of biodiversity. This study highlights the effects and severity of cultural eutrophication in Florida’s subtropical lakes.

The bigger picture: Managing carbon and removing it from the atmosphere (i.e., carbon sequestration) is an important aspect of climate mitigation. The carbon can be removed from the atmosphere and stored in places known as carbon sinks (natural environments that can absorb carbon dioxide from the atmosphere). This study shows that subtropical Florida lakes are effective carbon sinks for organic carbon that deserve to be protected from nutrient runoff that causes eutrophication.

Citation: Walters, M. N., Kenney, W. F., Brenner, M., and Webster, B. C. (2019). Organic carbon sequestration in sediments of subtropical Florida lakes. PLoS OnE 14(12), e0226273. doi: 10.1371/journal.pone.0226273

The Clues Ancient Glaciers Leave Behind on Mars

Transient post-glacial processes on Mars: Geomorphologic evidence for a paraglacial period

by: Erica R. Jawin, James W. Head, David R. Marchant 

Summarized by: Lisette Melendez

Figure 1: A map of the crater in the midlatitudes on Mars, showing the geologic features that were created due to deglaciation, like gullies and spatulate depressions. These same features can be found in post-glacial environments on Earth!

What data were used? Mars, just like Earth, goes through a cycle of glaciation and deglaciation. The rise and fall of glaciers on Mars is influenced primarily by the planet’s obliquity, or the tilt of its axis. During times of higher obliquity, the planet’s tilt is greater, hence its poles are exposed to more sunlight and the glaciers leave the poles and travel towards the middle of the planet. As the cycle continues and the tilt is lower, the glaciers leave the midlatitudes and migrate towards the poles once again. The period of time where environments are adjusting to deglaciation is known as a paraglacial period, and it comes with a group of identifying features that are well studied here on Earth. This study applies what we’ve learned about the kinds of geologic features that are left behind by glaciers on Earth to the environment on Mars. The area that is left behind by a glacier is known as a glacial deposit. By analyzing images of craters on Mars taken by cameras aboard the Mars Reconnaissance Orbiter, scientists are able to find evidence of paraglacial periods and how long they last on Mars.

Figure 2: A photo of two retreating glaciers in the Antarctic Valley that are leaving behind ridges that are comparable to the ones found on the Martian surface.

Methods:  After choosing a crater in the midlatitudes of Mars, the scientists began breaking down the features found in the images of the crater and mapping out the terrain, as shown in Figure 1. Glaciers leave behind special signatures in the rocks on Earth (e.g., here are some Time Scavengers posts about glacial geology on Earth: glaciers in Connecticut River Valley and glaciers in the Bay of Fundy), and the objective was to identify these same features on Mars. In order to further understand the processes that were occurring in the crater on Mars, analyses of places with the same climate and geologic features on Earth were used! The climate on Mars is arid and freezing, similar to the McMurdo Dry Valleys in Antarctica.

Figure 3: A diagram that shows the process of forming gullies and debris fans (piles of sediment), which can be seen in real-life in the next figure.

Results: Several geologic features that, when found together, are indicative of glaciers migrating away were found in this crater on Mars. Some of these features include ridges becoming increasingly deformed as one looks further downslope, as shown in Figure 2, where the ridges of the glacial deposits in Antarctica are more deformed at the bottom of the picture. Spoon-like holes, called spatulate depressions, were also found on both the Antarctic glacial deposits and the Martian crater, formed by ice weathering away. As glaciers retreat, they often leave behind steep slopes in their wake. These slopes are unstable, and over time, sediment flows downward and builds up on the sides to stabilize the slope, as shown in Figure 3. Gullies, which are a geologic feature formed by the path that the sediment took to travel downward, and the resulting triangular piles of sediment can be found both in the crater on Mars and on Earth, shown side by side in Figure 4.

Why is this study important? This study is important because it increases our understanding of the time frames of climate cycles on Mars, and also highlights the similarities and differences between Mars and Earth. On Earth, paraglacial periods are relatively short, and the features left behind are likely to be eroded away by rainfall, rivers, and vegetation. These features are better preserved on Mars, an extremely cold and dry planet that doesn’t have the same erosive forces.

Figure 4: An example of gullies and debris fans on Mars (left) and on Earth (right).

The big picture:  Understanding the formation of geologic features on Earth is essential to uncovering the geologic history of the rest of our planets. This study showed that several features that form after a glacier migrates away can be found both on Earth and on Mars. The key difference is the time frame: on Earth, the paraglacial period is relatively rapid, while on Mars, it takes place on the scale of millions of years. 

Citation:mJawin, E. R., Head, J. W. & Marchant, D. R. Transient post-glacial processes on Mars: Geomorphologic evidence for a paraglacial period. Icarus 309, 187–206 (2018).

Tracing the Body Plans of Echinoderms through Time

Evolution and Development at the Origin of a Phylum

by: Bradley Deline, Jeffrey R. Thompson, Nicholas S. Smith, Samuel Zamora, Imran A. Rahman, Sarah L. Sheffield, William I. Ausich, Thomas W. Kammer, and Colin D. Sumrall

Summarized by: Lisette Melendez

What data were used? In this paper, changes in the bodies of early echinoderms (the group that includes marine animals such as starfish and sea urchins!) are tracked in order to understand the trends that separate groups from the rest of the animal kingdom. The main question is: why are all the body plans so different from one another? Figure 1 shows the range of body plans for early echinoderms, but the distinction carries on even today, considering how starfish and sea cucumbers look so different from one another! In order to quantify these changes, the scientists directly studied specimens from various natural history museums, sifted through past echinoderm papers, discussed with experts in organism classification, and consulted the Treatise on Invertebrate Paleontology. Since the scientists were looking specifically at early echinoderms, we are talking about fossils that date back to the Cambrian and Ordovician periods, about 541-444 million years ago! Usually, data from fossils this old is limited because many significant characteristics are worn away with time. However, echinoderms have notable skeletons that retain a great deal of important characteristics, making their skeletons excellent indicators of evolutionary changes through time.

Figure 1: a collection of different early Paleozoic echinoderm body plans. The one featured in (A) is non-radial, (B) is pentaradial attached, (C) is mobile and able to move around freely, and (D) – (F) are pentaradial stalked (hence the stem-like structures).

Methods: Once all the data was gathered, the next step was to find a way to accurately portray the changes of early echinoderm bodies through time. A morphospace, or a representation of every possible shape of echinoderms, was created, as shown in Figure 2. Four major echinoderm body plans were revealed in the graph. Three of the groups had radial symmetry (symmetry around a central part), while one was non-radial. Two of the groups were characterized by stem-like stalks that attached the echinoderm to the sea floor, while another group was mobile and free to move around. While Figure 2 shows the overall body plans of early echinoderms, this graph was further broken down into specific time intervals (each about 20 million years long) in order to study how the body plans changed over time. Figure 3 depicts how different the body plans were from one another throughout time.

Results: By studying the graphs, several important evolutionary trends can be picked out. Take, for example, Figure 3. The Cambrian was when the first major echinoderm body plans appeared, but the Ordovician was really where each body plan became more complex and different from one another, pointing to the Great Ordovician Biodiversification Event. Each body plan became more well-defined over time, and the differences between the various body plans are highlighted by the extinction of the transitional forms that connected one body plan to another. Even as evolution continued to progress, sometimes certain species would “readapt” a characteristic that they lost thousands of millions of years previously, showing how flexible evolution can really be.               

Figure 2: A graph that shows all the different body types of Echinoderms, separated by characteristic differences like mobility and radial symmetry (or lack thereof).

Why is this study important?  This study is important in studying the mechanisms behind the nature of the Cambrian explosion: why do all of these major animal groups start appearing and how have the groups changed over time? This study shows how fluid characteristics are throughout time, with the introduction, removal, and possibly even a re-introduction of characteristics to body plans as time progresses (this is called homoplasy). It highlights the various patterns of body types within Echinodermata and the patterns of gaining or losing characteristics over time, indicating the complexity in studying how animals change over time.

Figure 3: A graph that shows the diversity of echinoderms between the Cambrian and the Ordovician (541 – 444 million years ago).

The big picture: This study helps us fill in some of the gaps in our knowledge about the Cambrian Explosion, a consequential chapter in the history of living creatures, and how animals have evolved since that point. It shows how evolution has changed the bodies of animals within the same group over time and helps us understand how some animals (like sand dollars and brittle stars) can look so different, yet be closely related to one another. 

 Citation: Deline et al., Evolution and Development at the Origin of a Phylum, Current Biology (2020), https://doi.org/10.1016/ j.cub.2020.02.054

The relationship between rodents and Homo floresiensis

Temporal shifts in the distribution of murine rodent body size classes at Liang Bua (Flores, Indonesia) reveal new insights into the paleoecology of Homo floresiensis and associated fauna

by: E. Grace Veatch, Matthew W. Tocheri, Thomas Sutikna, Kate McGrath, E. Wahyu Saptomo, Jatmiko, and Kristofer M. Helgen.

Summarized by: Kailey McCain

What data were used? Researchers once believed that Homo sapiens (i.e., modern humans) were the only hominid to reach the Indonesian islands. However, in the past few decades anthropologists, archeologists, and paleontologists have discovered an early hominid species’ cultural and skeletal remains, belonging to Homo floresiensis, on the island of Flores. Along with the hominid remains, 257,000 additional vertebrate skeletal elements were identified and 80% of the collected belonged to the murine rodent taxa (i.e., rats). The main rodent genera identified and used in this study varied in body size, which was used as a proxy (i.e., representative) to identify the paleoecology of the environment. The five genera used were: Papagomys, Spelaeomys, Hooijeromys, Komodomys, Paulamys, and Rattus (Figure 1).

Methods: The excavation site for the murine skeletal remains, as well as H. floresiensis, was within the Liang Bua, a limestone cave on Flores Island. The stratigraphy of Liang Bua was divided into sectors based on age, with the oldest being approximately 190-120 ka (thousand years ago) and the youngest sector at less than 3 ka. Once the sites were identified, researchers began excavating the remains by using a method called wet-sieving, which is the process of sediment separation using water to remove certain grain sizes and break apart agglomerates (i.e., a mass of sediment grains).

Once the murine remains were collected, researchers began identifying the different species by using molar and jaw sizes, as well as comparing the skeletal body to size to extant (i.e., living) rodents. In addition to dividing the remains into their different species, they were also further divided by size. The five distinct body size categories are: small (<100 g), medium (100-300 g), large (300-600 g), huge (600-1100 g), and giant (>1100 g).

Figure 1: This image represents how the different murine taxa, Papagomys, Spelaeomys, Hooijeromys, Komodomys, Paulamys, and Rattus, differ in body size and molar size.

Results: The data collected showed that the small and medium sized murines dominated the cave during the first two sectors (190-60 ka) but researchers noted a sharp decline in the medium sized murines during the 60-50 ka age range. This decrease in species can be correlated to the paleoclimate record, which indicated a substantial decrease in available vegetation. As time progressed to the age range 47-12 ka, researchers noticed no significant change in body size. This was a surprise to the researchers due to the geologic record indicating high levels of volcanic activity. The next range, 12-5 ka, exhibited a decrease in overall murine size that can be attributed to the high rainfall and monsoon season recorded for this time period. Finally, the age range 5-3 ka, showed the first increase of medium sized murines which could be correlated to the dispersal of Homo floresiensis and the subsequent opening of habitats, but will need further research to support the claim.

Why is this study important? This study is important because it shows the relationship between the dominant non-human animals and Homo floresiensis within the Liang Bua cave. Additionally, the researchers explored other ecological factors (e.g, weather, resource availability, volcanic activity) and showed how it affects not only the fauna in general, but showed the difference in responses between sizes.

Figure 2: This figure shows two images. Image (a.) shows researchers measuring a large modern cave rat, Papagomys armandvillei. Image (b.) shows a reconstructed image of H. floresiensis carrying a large rat over their shoulder.

The big picture: The researchers set out to determine the ways in which the dominant fauna, second to the hominid species, responded throughout time with the introduction and dispersal Homo floresiensis. While there was a relationship noted between murine size/distribution and hominid involvement, the data also suggested that additional ecological factors may have contributed; therefore, no significant conclusions can be made without additional research regarding the true impact of Homo floresiensis

Citation: Veatch, E. G., Tocheri, M. W., Sutikna, T., McGrath, K., Saptomo, E. W., & Helgen, K. M. (2019). Temporal shifts in the distribution of murine rodent body size classes at Liang Bua (Flores, Indonesia) reveal new insights into the paleoecology of Homo floresiensis and associated fauna. Journal of human evolution130, 45-60. https://doi.org/10.1016/j.jhevol.2019.02.002

Looking at past phosphorus accumulation in a Florida lake offers new insight on recent cultural nutrient enrichment

A Holocene Sediment Record of Phosphorus Accumulation in Shallow Lake Harris, Florida (USA) Offers New Perspectives on Recent Cultural Eutrophication

by: William F. Kenney, Mark Brenner, Jason H. Curtis, T. Elliott Arnold, Claire L. Schelske

Summarized by: Mckenna Dyjak

What data were used?: A 5.9 m sediment core was taken in Lake Harris, Florida using a piston corer (a technique used to take sediment samples, similar to how an apple is cored). Lake Harris is a subtropical, shallow, eutrophic body of water (rich with nutrients) located near Orlando, Florida.  

Methods: The 1.2 m sediment core is long enough to provide the complete environmental history of Lake Harris. However, the core must be interpreted first. In order to do so, the core was first dated using lead isotope 210Pb and carbon isotope 14C. The next steps involved using proxy data (preserved physical characteristics of the environment) to determine net primary productivity (the concentration and accumulation rates of organic matter), lake phosphorus enrichment (three forms of phosphorus), groundwater input (concentration and accumulation rates of carbonate material, like limestone), macrophyte abundance (e.g., sponge spicules), and phytoplankton abundance (e.g.,diatoms).

Results: The study found that Lake Harris began to fill with water in the early Holocene (~10,680 calendar years before the present) and transitioned to a wetter climate in the middle Holocene. The transition is indicated by a change in carbonate to organic sediments; a higher amount of organic sediments would suggest an increase in rainfall needed to support the plant life that would become the organic matter. A low sedimentation rate indicates that the lake was experiencing oligotrophication (depletion in nutrients) through the Holocene until around the 1900s. After the 1900s, there were increased sedimentation rates (Figure 1. A, B, D, and E) which indicates cultural eutrophication (increase of nutrients in bodies of water). Phosphates and nitrates from common fertilizers and other human activities (which is why it’s called “cultural eutrophication”) can allow algae (e.g., diatoms) to grow rapidly and reduce the amount of oxygen in the lake. An increased sedimentation rate can be used to determine whether a body of water is in a state of eutrophication, because the amount of phytoplankton (such as diatoms) would increase in accumulation. Total phosphorus accumulation rates can also indicate eutrophication.

Figure 1. Sedimentation rates for (A) bulk sediment, (B) organic matter, (C) CaCO3, (D) total phosphorus, (E) diatom biogenic silica and (F) sponge spicule biogenic silica versus core depth. Near the top of the core we can see a significant increase in A, B, D, E, and F which provide evidence for cultural eutrophication (increased sediment rates).

Why is this study important?: This study shows that, without being disturbed, Lake Harris was prone to becoming depleted in nutrients, the process of oligotrophication. The complete change of course due to human activities (i.e., fertilizer runoff) is more detrimental than was previously considered. This study showed that throughout the environmental history of Lake Harris there was never a sign of natural eutrophication, but rather that of oligotrophication. 

The bigger picture: Cultural eutrophication is a serious problem plaguing many aquatic systems and has serious consequences such as toxic algae blooms, which can have far reaching effects like on the tourism industry in Florida! The extent of damage caused by human activities is shown in this study and can help us understand how lakes responded in the past to the introduction of cultural eutrophication.  

Citation: Kenney WF, Brenner M, Curtis JH, Arnold TE, Schelske CL (2016) A Holocene Sediment Record of Phosphorus Accumulation in Shallow Lake Harris, Florida (USA) Offers New Perspectives on Recent Cultural Eutrophication. PLoS ONE 11(1): e0147331. https://doi.org/10.1371/journal.pone.0147331

Understanding how climate change affects predator-prey relationships in snails and clams

Climate-mediated changes in predator-prey interactions in the fossil record: a case study using shell-drilling gastropods from the Pleistocene Japan Sea

Tomoki Chiba and Shinichi Sato

Summarized by Baron Hoffmeister

What data were used? This study used a predator-prey analysis of drill holes found on fossil bivalve (clam) shells produced by gastropods (snails) found in the Oga Peninsula off the coast of Japan.

Methods: This study used computer analysis on fossil assemblages of bivalves to determine the location of predatory drill holes and the species of bivalves which indicated whether they are warm water dominant or cold water dominant species. The location of the drill holes on the bivalve shells was also analyzed to determine different predatory gastropods (Figure 1).

Figure 1. These are photographs of two predatory drill holes taken from a microscope. Section A-C is a predatory drill hole located on the center of the shell, and section D-F is a drill hole located on the shell edge. These two different types of predation patterns indicate two separate predatory gastropod species. Image from Chiba and Sato (2016).

Results: This study showed that drilling predation was influenced by the change of sea surface temperatures and sea level due to glacial-interglacial climate cycles. A glacial period occurs due to cool temperatures and glacial advancement, and an interglacial period occurs when glaciers retreat and sea level rises due to warming temperatures. As warm water currents decrease, so does the presence of warm-water predator gastropods. This causes them to shift their range, therefore changing rates of predator and prey interactions. In this study, predation slowed as seawater temperatures decreased and in turn found that this moderated the predation pressure between the gastropods and bivalve prey. This study also found that predator and prey interactions in a shallow-marine ecosystem are likely to weaken with cooling temperatures and strengthen with warming temperatures.

Why is this study important? This study indicates that predator-prey relationships can be used to help interpret changing climates and the implications it has on ecosystems. This study also notes that ocean climate variability has large implications of range shifts which can be used to interpret how organisms respond to changing climate conditions.

The big picture: The information found in this study can be used to help interpret current-day climate change and its influence on predator-prey relationships in relation to the biogeographical distribution of species due to ocean temperatures. This is useful for identifying ecosystems globally.

Citation:

Chiba, T., and Sato, S. I.. (2016). Climate-mediated changes in predator-prey interactions in the fossil record: a case study using shell-drilling gastropods from the Pleistocene Japan Sea. Paleobiology 42(2), 257–268. doi: 10.1017/pab.2015.38