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LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

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Page 1: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

LONG-TERM VEGETATIONAL CHANGE

IN A NEW YORK CITY

FRESHWATER WETLAND

Argie Miller, Dorothy Peteet, David Cruz

Page 2: 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

Page 3: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

• 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

Page 4: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

• Ice sheet melted, dropped huge chunks of ice

• Ice became buried in the outwash.

• Depressions filled with water and sediment.

Kettle Pond

Page 5: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

•Research Team:I.C.C Model Independence Critical Thinking Communication

•Coring with LivingstonPiston corer

• Stratigraphic examination

•200 cm deep sediment core

Methods

Page 6: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

EXAMINED:

•Preserved fossil seed/needle remains

•Charcoal particles • Sand and silt

Paleoecological Changes

Page 7: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

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)

Page 8: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

Macrofossils

Page 9: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

UPPER SAMPLES(Aquatics and emergent)

Potamogeton Brasenia NajasZannichellia

Macrofossils 1

Page 10: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

CAREX SPP

CYPERUS STRIGOSUS

SPARGANIUM

Macrofossils 2

LOWER SAMPLEViolaCarexPica (spruce) NeedleCyperus StrigosusSparganiumDaphnia egg case

Page 11: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

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.

Page 12: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

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

Page 13: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

• 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

Page 14: LONG-TERM VEGETATIONAL CHANGE IN A NEW YORK CITY FRESHWATER WETLAND Argie Miller, Dorothy Peteet, David Cruz

AcknowledgementsDorothy Peteet, PhD Principal InvestigatorDavid Cruz Student