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SE Coastal Plain and Piedmont

SE Coastal Plain and Piedmont

Southeastern Evergreen Forest

  • Longleaf, Loblolly, and Slash Pine

  • Maritime forest

  • Cypress-gum

  • Pocosin and Atlantic whitecedar

  • Bottomland hardwood

  • Hydrology, microtopography, soils, and disturbance are major factors that separate forest types from the Coastal Plain.

  • Live oak (Quercus virginiana)

Maritime Forest

  • Forest structure

  • Species composition

    • Canopy

      • Live oak, loblolly pine, sand laurel oak

    • Shrubs

      • Yaupon holly, eastern redcedar, waxmyrtle

    • Understory/herb layer—sparse

  • Wildlife value

  • Environmental factors

    • Disturbance

    • Temperature/precipitation not selective factors

    • Sandy soils

    • Wind and storms

    • Salt spray and overwash (forms thick canopy layer to protect from salt spray)

  • Disturbance regime

  • Threats

    • Development

    • Climate change, especially sea level rise (ghost forests)

  • Which direction are we looking (north or south)?

      • North (ocean is East)

  • What are the key environmental factors that shape maritime forests?

Cypress-Gum Forests

  • Forest structure

    • often adjacent to bottomland sites

    • wettest of the coastal plain forest types; often flooded 3-6 months

    • Canopy of flood-tolerant species

    • Understory limited

    • No herbaceous layer

  • Species composition

    • Brownwater swamps (more widespread)

      • Baldcypress and Nyssa biflora (smaller leaves than blackgum)

    • Blackwater swamps

      • Blackcypress and Nyssa aquatica

    • Other species: Carolina ash, red maple, black gum

  • Environmental factors

    • Flooded in winter and early spring; flooded 3-6 months of the year

    • Flooding is the major selective factor that determines what species can survive

  • Disturbance regime

    • No cycle of regular natural disturbance; no fire

    • Hurricanes are periodic

    • Can be very long-lived

  • Threats

    • Climate change and saltwater intrusion

Carolina Bays, Pocosins, and Atlantic whitecedar

  • IMPORTANT: While the origin of the word “pocosin” is Algonquin, it does NOT translate to “swamp on a hill.” It is a generic term that refers to a wet area

  • Carolina bays describe some SE coastal plain geography; pocosins and Atlantic whitecedar are 2 community types found in Carolina Bays. Pocosins are closely related to Bay Forests.

Carolina Bays

  • Elliptical bays that either have open water or wetland forests

  • NW-SE orientation

  • Mostly organic soils and “bay” forests (either pocosin or Atlantic whitecedar)

  • Sandy rim (xeric longleaf pine forest) on the SE rims

  • Many have been drained and converted to agriculture

  • Ongoing debate about origin and formation

  • Carolina bays were thought to have formed through wind and weather patterns

  • Both types share seasonally wet, organic soils

  • The main difference (we think) is the disturbance regime

    • Pocosin and Bay Forests—moderate fire regime (about 10 year cycle)

    • Atlantic whitecedar—infrequent but catastrophic fire

Pocosin or Bay Forest

  • Environmental factors

    • Organic soils, from a few feet to 12 ft deep

    • Bays and depression ponds fill with partially decayed leaves, turns into “muck”

    • Organic soils hold water like a sponge

  • Forest structure

    • Canopy often open—also described as an evergreen shrub bog

    • Drier sites have trees and are called Bay Forests

      • Thick and evergreen midstory or understory of “bay” species

      • Often woven together with vines

      • Little herbaceous understory

  • Species composition

    • Canopy

      • Pond pine, Pinus serotina

    • Understory/shrub layer

      • Bay species: titi, sweetbay magnolia, swampbay, loblollybay

    • Vines weave everything together in a thick tangle

  • Disturbance - 10 year fire cycle

    • Pond pine: fire adapted: serotinous cones, epicormic branching, thick bark to withstand some fire

  • Threats

    • Former threats: ditching and draining for land conversion

    • Now: fire suppression, climate change

Atlantic Whitecedar Forests

  • Forest structure and disturbance regime

    • used to exist in pure, even-ages stands

    • remaining stands like this are rare; some found in the Albemarle/Pamlico penninsula in NC

    • even-aged structure suggest that catastrophic disturbance is needed for regeneration

    • Fire cycle through to be > 50 years

    • Large plant biomass = hot fires, clears seed bed

    • Selective cutting converted forests to gum and red maple

  • Species composition:

    • Atlantic whitecedar

Fire as a selective mechanism in the SE Coastal Plain

  • Frequent, low-intensity

    • longleaf pine

    • plants are adapted to survive fire

      • seed germination during non-fire season (fall)

      • grass stage

      • long, lush protective needles

      • loss of dead branches

      • thick bark

  • Infrequent, high-intensity

    • Atlantic whitecedar

    • plants can regenerate after fire

      • serotinous cones

      • abundant cone production; precocious (produce cones early)

      • short needles

      • dead branches retained (ladder)

      • thin bark

  • Longleaf pine, pondpine, and whitecedar are all shade intolerant with different adaptations

Bottomland Hardwood Forests

  • Forest structure

    • Geography: adjacent to brown or blackwater rivers, with periodic flooding

    • Closed canopy

    • Understory variable but uneven-aged, can be shrubby

    • Herb layer may or may not be rich

  • Species composition

    • Brownwater rivers

      • higher diversity; nutrient-rich sediment

      • Oaks dominant

      • Also green ash, sweetgum, American elm, musclewood

    • Blackwater rivers

      • Quercus laurifolia and Pinus taeda dominant

      • Understory: Magnolia virginiana, Persea palustris, Cyrilla racemiflora

  • Environmental factors

    • Brownwater rivers (also called redwater rivers)—originate in the Piedmont or Mountains, contain sediment

    • Blackwater rivers: originate in the Coastal Plain, lack sediment, but high in tannins—acidic, dark, and clear

    • Which type has a greater diversity of species? → Brownwater (blackwater is acidic and lacks sediment)

    • Wet and low-lying

    • Fires are not a factor (too wet to burn)

    • important habitat for birds like prothonotary warbler

    • Notice, also, that the species in brownwater Bottomland Hardwoods are common species of the Piedmont, and (not surprisingly), blackwater Bottomland Hardwoods have species that are more restricted to the Coastal Plain.

  • Disturbance regime

    • logged extensively for valuable timber

    • hurricanes

  • Threats

    • Habitat loss

      • conversion to agriculture

      • timber harvest

      • development

    • Invasive species

      • emerald ash borer

R

SE Coastal Plain and Piedmont

SE Coastal Plain and Piedmont

Southeastern Evergreen Forest

  • Longleaf, Loblolly, and Slash Pine

  • Maritime forest

  • Cypress-gum

  • Pocosin and Atlantic whitecedar

  • Bottomland hardwood

  • Hydrology, microtopography, soils, and disturbance are major factors that separate forest types from the Coastal Plain.

  • Live oak (Quercus virginiana)

Maritime Forest

  • Forest structure

  • Species composition

    • Canopy

      • Live oak, loblolly pine, sand laurel oak

    • Shrubs

      • Yaupon holly, eastern redcedar, waxmyrtle

    • Understory/herb layer—sparse

  • Wildlife value

  • Environmental factors

    • Disturbance

    • Temperature/precipitation not selective factors

    • Sandy soils

    • Wind and storms

    • Salt spray and overwash (forms thick canopy layer to protect from salt spray)

  • Disturbance regime

  • Threats

    • Development

    • Climate change, especially sea level rise (ghost forests)

  • Which direction are we looking (north or south)?

      • North (ocean is East)

  • What are the key environmental factors that shape maritime forests?

Cypress-Gum Forests

  • Forest structure

    • often adjacent to bottomland sites

    • wettest of the coastal plain forest types; often flooded 3-6 months

    • Canopy of flood-tolerant species

    • Understory limited

    • No herbaceous layer

  • Species composition

    • Brownwater swamps (more widespread)

      • Baldcypress and Nyssa biflora (smaller leaves than blackgum)

    • Blackwater swamps

      • Blackcypress and Nyssa aquatica

    • Other species: Carolina ash, red maple, black gum

  • Environmental factors

    • Flooded in winter and early spring; flooded 3-6 months of the year

    • Flooding is the major selective factor that determines what species can survive

  • Disturbance regime

    • No cycle of regular natural disturbance; no fire

    • Hurricanes are periodic

    • Can be very long-lived

  • Threats

    • Climate change and saltwater intrusion

Carolina Bays, Pocosins, and Atlantic whitecedar

  • IMPORTANT: While the origin of the word “pocosin” is Algonquin, it does NOT translate to “swamp on a hill.” It is a generic term that refers to a wet area

  • Carolina bays describe some SE coastal plain geography; pocosins and Atlantic whitecedar are 2 community types found in Carolina Bays. Pocosins are closely related to Bay Forests.

Carolina Bays

  • Elliptical bays that either have open water or wetland forests

  • NW-SE orientation

  • Mostly organic soils and “bay” forests (either pocosin or Atlantic whitecedar)

  • Sandy rim (xeric longleaf pine forest) on the SE rims

  • Many have been drained and converted to agriculture

  • Ongoing debate about origin and formation

  • Carolina bays were thought to have formed through wind and weather patterns

  • Both types share seasonally wet, organic soils

  • The main difference (we think) is the disturbance regime

    • Pocosin and Bay Forests—moderate fire regime (about 10 year cycle)

    • Atlantic whitecedar—infrequent but catastrophic fire

Pocosin or Bay Forest

  • Environmental factors

    • Organic soils, from a few feet to 12 ft deep

    • Bays and depression ponds fill with partially decayed leaves, turns into “muck”

    • Organic soils hold water like a sponge

  • Forest structure

    • Canopy often open—also described as an evergreen shrub bog

    • Drier sites have trees and are called Bay Forests

      • Thick and evergreen midstory or understory of “bay” species

      • Often woven together with vines

      • Little herbaceous understory

  • Species composition

    • Canopy

      • Pond pine, Pinus serotina

    • Understory/shrub layer

      • Bay species: titi, sweetbay magnolia, swampbay, loblollybay

    • Vines weave everything together in a thick tangle

  • Disturbance - 10 year fire cycle

    • Pond pine: fire adapted: serotinous cones, epicormic branching, thick bark to withstand some fire

  • Threats

    • Former threats: ditching and draining for land conversion

    • Now: fire suppression, climate change

Atlantic Whitecedar Forests

  • Forest structure and disturbance regime

    • used to exist in pure, even-ages stands

    • remaining stands like this are rare; some found in the Albemarle/Pamlico penninsula in NC

    • even-aged structure suggest that catastrophic disturbance is needed for regeneration

    • Fire cycle through to be > 50 years

    • Large plant biomass = hot fires, clears seed bed

    • Selective cutting converted forests to gum and red maple

  • Species composition:

    • Atlantic whitecedar

Fire as a selective mechanism in the SE Coastal Plain

  • Frequent, low-intensity

    • longleaf pine

    • plants are adapted to survive fire

      • seed germination during non-fire season (fall)

      • grass stage

      • long, lush protective needles

      • loss of dead branches

      • thick bark

  • Infrequent, high-intensity

    • Atlantic whitecedar

    • plants can regenerate after fire

      • serotinous cones

      • abundant cone production; precocious (produce cones early)

      • short needles

      • dead branches retained (ladder)

      • thin bark

  • Longleaf pine, pondpine, and whitecedar are all shade intolerant with different adaptations

Bottomland Hardwood Forests

  • Forest structure

    • Geography: adjacent to brown or blackwater rivers, with periodic flooding

    • Closed canopy

    • Understory variable but uneven-aged, can be shrubby

    • Herb layer may or may not be rich

  • Species composition

    • Brownwater rivers

      • higher diversity; nutrient-rich sediment

      • Oaks dominant

      • Also green ash, sweetgum, American elm, musclewood

    • Blackwater rivers

      • Quercus laurifolia and Pinus taeda dominant

      • Understory: Magnolia virginiana, Persea palustris, Cyrilla racemiflora

  • Environmental factors

    • Brownwater rivers (also called redwater rivers)—originate in the Piedmont or Mountains, contain sediment

    • Blackwater rivers: originate in the Coastal Plain, lack sediment, but high in tannins—acidic, dark, and clear

    • Which type has a greater diversity of species? → Brownwater (blackwater is acidic and lacks sediment)

    • Wet and low-lying

    • Fires are not a factor (too wet to burn)

    • important habitat for birds like prothonotary warbler

    • Notice, also, that the species in brownwater Bottomland Hardwoods are common species of the Piedmont, and (not surprisingly), blackwater Bottomland Hardwoods have species that are more restricted to the Coastal Plain.

  • Disturbance regime

    • logged extensively for valuable timber

    • hurricanes

  • Threats

    • Habitat loss

      • conversion to agriculture

      • timber harvest

      • development

    • Invasive species

      • emerald ash borer

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