@ARTICLE{TreeBASE2Ref16146,
author = {Michael Knapp and Ragini Mudaliar and David Havell and Steven J. Wagstaff and Peter J. Lockhart},
title = {The Drowning of New Zealand and the Problem of Agathis.},
year = {2007},
keywords = {},
doi = {10.1080/10635150701636412},
url = {},
pmid = {},
journal = {Systematic Biology},
volume = {56},
number = {5},
pages = {862--870},
abstract = {80 million years ago (mya) the landmass that was to become New Zealand broke away from the Gondwanan super continent. During the Oligocene period (26 - 38 mya) there was a significant reduction in the landmass of New Zealand However, whether or not New Zealand was completely submerged is a matter of controversy and recent debate. If it was completely submerged during the Oligocene, then all extant biota must have arrived by transoceanic distance dispersal since that time. This study reports molecular systematic and molecular clock analyses based on 3011 base pairs of sequence data (matK and rbcL coding regions, trnD-trnT intergenic region) from the chloroplast genome of nine different species from the Araucariaceae family. Analyses of these data suggest that Australian and New Zealand Agathis lineages diverged in the late Cretaceous/early Tertiary period. These estimates are consistent with in situ survival of the Agathis australis lineage in New Zealand following the breakup of Gondwana. They imply the continuous existence of land in the New Zealand area throughout the Tertiary.}
}
Citation for Study 1869
Citation title:
"The Drowning of New Zealand and the Problem of Agathis.".
This study was previously identified under the legacy study ID S1844
(Status: Published).
Citation
Knapp M., Mudaliar R., Havell D., Wagstaff S., & Lockhart P. 2007. The Drowning of New Zealand and the Problem of Agathis. Systematic Biology, 56(5): 862-870.
Authors
-
Knapp M.
-
Mudaliar R.
-
Havell D.
-
Wagstaff S.
-
Lockhart P.
Abstract
80 million years ago (mya) the landmass that was to become New Zealand broke away from the Gondwanan super continent. During the Oligocene period (26 - 38 mya) there was a significant reduction in the landmass of New Zealand However, whether or not New Zealand was completely submerged is a matter of controversy and recent debate. If it was completely submerged during the Oligocene, then all extant biota must have arrived by transoceanic distance dispersal since that time. This study reports molecular systematic and molecular clock analyses based on 3011 base pairs of sequence data (matK and rbcL coding regions, trnD-trnT intergenic region) from the chloroplast genome of nine different species from the Araucariaceae family. Analyses of these data suggest that Australian and New Zealand Agathis lineages diverged in the late Cretaceous/early Tertiary period. These estimates are consistent with in situ survival of the Agathis australis lineage in New Zealand following the breakup of Gondwana. They imply the continuous existence of land in the New Zealand area throughout the Tertiary.
External links
About this resource
- Canonical resource URI:
http://purl.org/phylo/treebase/phylows/study/TB2:S1869
- Other versions:
Nexus
NeXML
- Show BibTeX reference
@ARTICLE{TreeBASE2Ref16146,
author = {Michael Knapp and Ragini Mudaliar and David Havell and Steven J. Wagstaff and Peter J. Lockhart},
title = {The Drowning of New Zealand and the Problem of Agathis.},
year = {2007},
keywords = {},
doi = {10.1080/10635150701636412},
url = {},
pmid = {},
journal = {Systematic Biology},
volume = {56},
number = {5},
pages = {862--870},
abstract = {80 million years ago (mya) the landmass that was to become New Zealand broke away from the Gondwanan super continent. During the Oligocene period (26 - 38 mya) there was a significant reduction in the landmass of New Zealand However, whether or not New Zealand was completely submerged is a matter of controversy and recent debate. If it was completely submerged during the Oligocene, then all extant biota must have arrived by transoceanic distance dispersal since that time. This study reports molecular systematic and molecular clock analyses based on 3011 base pairs of sequence data (matK and rbcL coding regions, trnD-trnT intergenic region) from the chloroplast genome of nine different species from the Araucariaceae family. Analyses of these data suggest that Australian and New Zealand Agathis lineages diverged in the late Cretaceous/early Tertiary period. These estimates are consistent with in situ survival of the Agathis australis lineage in New Zealand following the breakup of Gondwana. They imply the continuous existence of land in the New Zealand area throughout the Tertiary.}
}
- Show RIS reference
TY - JOUR
ID - 16146
AU - Knapp,Michael
AU - Mudaliar,Ragini
AU - Havell,David
AU - Wagstaff,Steven J.
AU - Lockhart,Peter J.
T1 - The Drowning of New Zealand and the Problem of Agathis.
PY - 2007
KW -
UR - http://dx.doi.org/10.1080/10635150701636412
N2 - 80 million years ago (mya) the landmass that was to become New Zealand broke away from the Gondwanan super continent. During the Oligocene period (26 - 38 mya) there was a significant reduction in the landmass of New Zealand However, whether or not New Zealand was completely submerged is a matter of controversy and recent debate. If it was completely submerged during the Oligocene, then all extant biota must have arrived by transoceanic distance dispersal since that time. This study reports molecular systematic and molecular clock analyses based on 3011 base pairs of sequence data (matK and rbcL coding regions, trnD-trnT intergenic region) from the chloroplast genome of nine different species from the Araucariaceae family. Analyses of these data suggest that Australian and New Zealand Agathis lineages diverged in the late Cretaceous/early Tertiary period. These estimates are consistent with in situ survival of the Agathis australis lineage in New Zealand following the breakup of Gondwana. They imply the continuous existence of land in the New Zealand area throughout the Tertiary.
L3 - 10.1080/10635150701636412
JF - Systematic Biology
VL - 56
IS - 5
SP - 862
EP - 870
ER -
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