PHILIPPINE BIOGEOGRAPHY Flashcards
(61 cards)
What are the three tectonic plates
Philippine Sea Plate
Eurasian Plate
Sunda Plate
These groups encompass over 7,600 islands.
What plate?
(particularly the microcontinental block of Palawan); shares geological affinity with southern China and the rest of Sundaland.
Sunda Plate
This indicates a high level of biodiversity unique to the Philippines.
What role does the Philippine Sea Plate play in the geological formation of the Philippines?
Shapes eastern Luzon, Samar, and Mindanao
It is one of the tectonic plates contributing to the archipelago’s formation.
Eurasian plate contributes to the formation of the (2)
Central Cordillera and Sierra Madre mountain ranges
This trench is where the Eurasian Plate dives beneath Luzon.
- were formed by the subduction zones.
- not only cause earthquakes and volcanoes, but also drive the emergence of new islands and influence species evolution, shaping the Philippines into a biogeographic hotspot.
Trenches
What are the two trenches
Philippine Trench
Manila Trench
What is the Philippine Trench?
A subduction zone where the Philippine Sea Plate is subducting westward
It is located east of the Philippine islands.
trench at west, represents the Eurasian Plate diving beneath Luzon
Manila Trench
Some of these blocks, like ________ and ________, were once part of the Sundaland continent
Palawan and Mindoro
Timeline:
~45–30 Ma (Eocene to Mid Oligocene)
~30 Ma (Mid Oligocene)
~20 Ma (Early Miocene)
~15–10 Ma (Middle to Late Miocene)
~10–15 Ma
~5 Ma (Early Pliocene)
~45–30 Ma (Eocene to Mid Oligocene): Palawan forms as part of the Sunda Shelf (North Palawan Block).
~30 Ma (Mid Oligocene):
Proto-Luzon and Visayan terranes begin forming through tectonic collisions and subduction.
Mostly submerged under shallow seas — not yet suitable for terrestrial life.
Mindoro forms as a transitional continental fragment (North Palawan Block), possibly emerging shortly after Palawan.
~20 Ma (Early Miocene):
Eastern Luzon, including the Sierra Madre range, starts to rise above sea level.
First opportunities for biological colonization by flying organisms (e.g., birds, insects).
Formation of habitable volcanic islands begins in the Philippine Mobile Belt.
~15–10 Ma (Middle to Late Miocene):
Visayan islands begin to emerge above sea level.
Increasingly fragmented island landscapes develop.
Opportunities for dispersal, isolation, and early speciation grow.
~10–15 Ma:
Visayan islands begin emerging above sea level.
Increasingly complex island landscapes form.
~5 Ma (Early Pliocene):
Eastern Mindanao terranes rise above sea level.
Final major pieces of the modern Philippine archipelago fall into place.
Full establishment of isolated evolutionary “island arenas”.
What is the significance of PAICs in biogeography?
- Explain species distribution and evolutionary isolation.
- Support high levels of endemism in the Philippines.
- Useful framework for conservation planning and protected area design.
- Help trace evolutionary history and faunal migration patterns.
PAICs support high levels of endemism and are useful in conservation planning.
What does PAIC stand for?
Pleistocene Aggregate Island Complex
PAICs were groups of islands connected during the Pleistocene epoch.
List the major PAICs in the Philippines.
- Greater Luzon PAIC
- Greater Mindanao PAIC
- Greater Palawan PAIC
- Greater Negros–Panay PAIC
- Greater Sulu PAIC
These PAICs reflect historical land connections during glacial periods.
Greater Luzon PAIC
Luzon, Polillo Islands, Marinduque, Catanduanes
Includes unique species like the Luzon Tree Mouse and Luzon Bleeding-heart Dove.
Greater Mindanao PAIC
Mindanao, Leyte, Samar, Bohol, Camiguin
It supports unique species like the Tamaraw and Mindoro Short-legged Skink.
Greater Palawan PAIC
Palawan, Balabac, Busuanga, Culion
Greater Negros–Panay PAIC
Negros, Panay, Guimaras, Masbate, Cebu, Ticao
Greater Sulu PAIC
Basilan, Jolo, Tawi-Tawi, Pangutaran
MINOR PAICS
- Mindoro PAIC: Mindoro Island (not connected to Luzon or Palawan during the Pleistocene)
- Romblon PAIC: Romblon Islands (Sibuyan, Tablas, Romblon)
- Babuyan PAIC: Babuyan Islands north of Luzon (e.g., Calayan, Camiguin Norte)
- Batanes PAIC (sometimes treated separately): Batan Island, Itbayat, Sabtang (distinct biogeographic origin)
- Sibutu–Simunul PAIC (borderline PAIC near Borneo): Sibutu and Simunul (now politically part of Tawi-Tawi but historically distinct)
Formation: These islands were connected during glacial sea-level lows. Luzon formed from volcanic island arcs and accreted terrains during the Cenozoic.
Geological Background: Proto-Luzon originated from volcanic activity; it merged with other blocks over time.
Greater Luzon PAIC
Formation: These Visayan islands were once connected to Mindanao due to lower sea levels.
Geological Background: Formed through subduction-related volcanism and the tectonic compression of the Philippine Mobile Belt.
Greater Mindanao PAIC
Formation: Was never submerged entirely and became connected to Borneo during glacial maxima.
Geological Background: Continental origin (not volcanic); Palawan rifted from the Asian mainland in the Oligocene
Greater Palawan PAIC
Formation: Connected during glacial periods; land bridges joined these islands due to lowered sea levels.
Geological Background: Mostly volcanic, part of the Visayan arc, uplifted through subduction dynamics.
Greater Negros–Panay PAIC
Formation: These islands formed a single landmass during the Pleistocene glacial maxima.
Geological Background: Volcanic island arc related to the Sulu Trench subduction system.
Greater Sulu PAIC