long-term vegetational change in a new york city freshwater wetland
DESCRIPTION
LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz. Services of Wetlands. Carbon storage pools in the global carbon cycle Preserve water quality and water supply Protection against flooding and erosion - PowerPoint PPT PresentationTRANSCRIPT
LONG-TERM VEGETATIONAL CHANGE
IN A NEW YORK CITY
FRESHWATER WETLAND
Argie Miller, Dorothy Peteet, David Cruz
• Carbon storage pools in the global carbon cycle
• Preserve water quality and water supply
• Protection against flooding and erosion
• Essential habitat for fish and wildlife
• Archives for paleoecology
Services of Wetlands
• Three Kettle Ponds Lilly, Decodon, and Turtle
Ponds
• 15,000 years old
• Glacial-age remnant
Alley Pond Park (40o45’21.55”N; 73o45’38”W)
Queens, NY
• Ice sheet melted, dropped huge chunks of ice
• Ice became buried in the outwash.
• Depressions filled with water and sediment.
Kettle Pond
•Research Team:I.C.C Model Independence Critical Thinking Communication
•Coring with LivingstonPiston corer
• Stratigraphic examination
•200 cm deep sediment core
Methods
EXAMINED:
•Preserved fossil seed/needle remains
•Charcoal particles • Sand and silt
Paleoecological Changes
0.00 0.10 0.20 0.30
9
44
79
109
147
Density (g/cc)
De
pth
(c
m)
Turtle Pond Core 1 Organic/Inorganic Density
Organic matter Inrganic matter
0.00 0.10 0.20 0.30
9
44
79
109
147
Density (g/cc)
De
pth
(c
m)
Turtle Pond Core 1 Organic/Inorganic Density
Organic matter Inrganic matter
0.00 0.10 0.20 0.30 0.40 0.50
10
48
87
103
116
129
Density (g/cc)
De
pth
(cm
)
Turtle Pond Core 2 Organic/Inorganic Density
Organic matter Inrganic matter
Loss onIgnition
(LOI)
Macrofossils
UPPER SAMPLES(Aquatics and emergent)
Potamogeton Brasenia NajasZannichellia
Macrofossils 1
CAREX SPP
CYPERUS STRIGOSUS
SPARGANIUM
Macrofossils 2
LOWER SAMPLEViolaCarexPica (spruce) NeedleCyperus StrigosusSparganiumDaphnia egg case
Macrofossils 3 Charcoal Fragments
•suggest a large increase in fire near the pond above 20cm •At lower depths, a steady low pattern of accumulation
Sand•Sand abundance was variable •highest at 160-140 cm depth.
Results Increasing organic matter in upper sediments, suggesting wetter environment, possibly wetter climate.
Questions1.Why is deposition rate so low, if kettle? why not 10 meters deep, like nearby Alpine Swamp in New Jersey or Moravian Swamp, Staten I?
2.How old is spruce needle at bottom? Does it represent boreal forest after ice melt, or Little Ice Age more recently? Spruce does not occur naturally in NYC today
• Records of climate change in New York City region are sparse.
• Research needed to document rates of change and human impact
• Compare natural frequencies of fire to human-induced fire activity.
Conclusions
AcknowledgementsDorothy Peteet, PhD Principal InvestigatorDavid Cruz Student