News | March 4, 2014
An ecosystem feels the human touch
The scientists were able to track how the ecosystem has changed during recent periods in Earth's history, including the Medieval Warm Period (MWP) and the Little Ice Age (LIA). They compared what they saw to more recent changes brought about by humankind. The results highlight just how dramatic a force of change humans can be on planet Earth.
Recently, a team of scientists drilled into the HRNERR and collected core samples that provide a geological record of the region over the past 1100 years (roughly since the year 900). This "stratigraphic paleo-ecological" column can basically be read like a book by scientists who want to know more about how this beautiful ecosystem has changed over time in response to environmental pressures — be it changes in Earth's climate or the arrival of human industry in the region.
When looking at the sediment cores, the scientists search for a number of different clues about what the environment of the HRNERR has gone through over the centuries. First, they look at the signs of life contained within the cores — such as pollen, spores and fossils. This material from ancient plants and animals sinks to the bottom of the marsh and ends up trapped in the layers of sediments, thereby providing us with direct evidence of what lived on the site.
When the research team opened the geological book written by the HRNERR, they spotted specific eras of history. The Medieval Warm Period (MWP) was the first — a time of warm and dry weather in the north Atlantic that lasted from about A.D. 800 to 1300. Evidence of erosion in the sediment samples indicates that vegetation in the region, and the roots that held the soil in place, died off during the drought. Water in the region grew scarce, evaporation in the heat increased, and plants that were adapted to saltier climates moved in.
Next came the Little Ice Age (LIA) that lasted from the early 1400s to the late 1800s. This period in human history marked centuries of cold, wet weather, and the evidence of local vegetation in the sediments also changed along with the climate.
And then came a flood of human influence. When Europeans arrived on the east coast of America, they brought with them dramatic changes to land use. This area is now one of the most heavily populated regions in the world. Urban landscapes dominate from New York to Boston (and indeed south past Washington DC). The results of this urbanization can also be seen in the sediments.
With samples of three periods of climate change in their hands, the researchers asked, "Which events have had the greatest influence on this ecosystem?" Was it global cooling or drought that caused the largest disruption in plant and animal species … or was it factories and farming?
The answer, it seems, points the finger firmly in humankind's direction. According to the researchers, "The large magnitude of shifts in vegetation, sedimentation, and nutrients during the last few centuries suggests that human activities have made the greatest impact to the marshes of the Hudson Estuary during the last millennium."
This is not an unfamiliar conclusion. Other marsh studies in the northeastern and Mid-Atlantic states have revealed a similar signature of humankind stamped into the geologic history of the region.
"We see this pattern in our marsh studies throughout the Hudson Estuary, as well as in lakes and bogs in the region," says Dr. Dorothy Peteet of the NASA Goddard Institute for Space Studies and co-author on the study. "The vegetational shifts are dramatic in the marshes with human impact, because of the pattern of invasive species that create monocultures, such as Typha (cattails) and Phragmites (common reed) which are present in all of them. We have published several studies regionally that show a similar pattern, from the very large Hackensack Meadowlands, N.J. and Jamaica Bay, N.Y. northward in Piermont, Iona Marsh, and Sutherland Fen and Rhododendron Swamp, N.Y. upriver."
The study provides important information about how distinct periods of climate change affect this ecosystem. More importantly, it also shows us how dramatic and widespread the damage from human activities can be to ecosystems when compared to the changes that occur as a result of the natural variations in climate that the Earth experiences.
"While the past shifts in climate such as the Little Ice Age and the Medieval Warm Interval have shifted native plants in a natural way," Dr. Peteet explains. "What we see now in the marsh and lake records are invasive takeovers of the native vegetation due to shifts in human impact on nutrients, primarily heavy nitrogen fertilization."
Studying how this ecosystem has changed over time has important implications for the future of the HRNERR.
"Studies such as this paleo-ecological history of Tivoli Bays are particularly important for wetland restoration," says Dr. Peteet. "Previously, it was thought that a Phragmites wetland should be restored to a cattail wetland, but our studies show that often cattails were also invaders, and that native plants such as sedges are key to a healthy, productive native wetland."
The results, when viewed alongside similar studies from other parts of the world, are also providing insight into the more global effects of humankind.
"This pattern of higher nutrients leading to different vegetation growth is a global one, and a problem that is growing … not only for marsh wetlands, but also for many peat bogs in Europe," says Dr. Peteet.
NASA News: Marshes Tell Story of Medieval Drought, Little Ice Age, and European Settlers near New York City
NYS DEC: Hudson River National Estuarine Research Reserve
Sritrairat, S., D.M. Peteet, T.C. Kenna, R. Sambrotto, D. Kurdyla, and T. Guilderson, 2012: A history of vegetation, sediment and nutrient dynamics at Tivoli North Bay, Hudson Estuary, New York. Estuar. Coast. Shelf Sci., 102, 24-35, doi:10.1016/j.ecss.2012.03.003.
This article was originally prepared as a feature for Astrobiology Magazine.