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Data from: Sea level change and the area of shallow-marine habitat: implications for marine biodiversity
负责人:
关键词:
diversity;transgression;regression;Species-Area Relationship;sea level
DOI:
doi:10.5061/dryad.4pt8h
摘要:
complicated relationship. In contrast to prevailing views, sea-level rise does not consistently generate an increase in shelf area, nor does sea-level fall
Data from: Leaf form and photosynthetic physiology of Dryopteris species distributed along light gradients in eastern North America
负责人:
关键词:
Comparative Methods;Dryopteris;hydraulics;photosynthetic light response;polyploidy;Ferns;transgressive trait expression;gas exchange;Holocene;light regimes
DOI:
doi:10.5061/dryad.38h06
摘要:
and physiological variation. Allopolyploid hybrids did not show transgression in any physiological parameter that may have allowed them to coexist regionally
Data from: Climate and sea-level changes across a shallow marine Cretaceous–Palaeogene boundary succession in Patagonia, Argentina
负责人:
关键词:
Paleogene;sea-level;K-Pg boundary;climate;biostratigraphy;Cretaceous;sea level;dinocysts
DOI:
doi:10.5061/dryad.r86pk
摘要:
ing in a hiatus directly at the boundary in both sections, followed by a transgression in the Danian.
Data from: Did post-glacial sea-level changes initiate the evolutionary divergence of a Tasmanian endemic raptor from its mainland relative?
负责人:
关键词:
Last Glacial Maximum;inbreeding depression;Aquila audax;Quaternary;marine dispersal;vicariance;sea level;subspecies
DOI:
doi:10.5061/dryad.tc88k
摘要:
marine transgression as the initiator of divergence of terrestrial lineages on continental islands and adjacent mainland, and highlight the ra
North American stage boundary in the Wilberns and Tanyard Formations of central Texas
负责人:
关键词:
Lingulella;Wahwahlingula;Schizambon;Eurytreta sublata;Ordovician;biomere;Cambrian;extinction;Stitta notchensis;Stittia ornata;Schizambon langei;Siphonobolus;Quadrisonia lavadamensis;linguliform brachiopod;Zhanatella utahensis
DOI:
doi:10.5061/dryad.64td7
摘要:
ng a transgression. The disappearance of the Sunwaptan fauna and the arrival of the Skullrockian fauna are distinct events. We suggest that “biomere” events ma

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