The combined effect of sea level and supply during Milankovitch cyclicity: Evidence from shallow-marine δ18O records and sequence architecture (Adriatic margin)

Geology

Volumn 37, Issue 11, 2009, Pages 1003-1006

  Ridente, Domenico ^a   Trincardi, F ^b   Piva, A ^b   Asioli, A ^c  

^a SAPIENZA UNIVERSITY OF ROME   (Italy)

^b ISMAR CNR   (Italy)

^c CNR   (Italy)

Author keywords

[No Author keywords available]

Indexed keywords

ADRIATIC; BENTHIC FORAMINIFERA; BUILDING BLOCKES; CHRONOSTRATIGRAPHIC DATA; COMBINED EFFECT; COMPOSITE CLIMATE; CYCLICITY; DEPOSITIONAL SEQUENCES; GLACIAL-INTERGLACIAL CYCLES; IN-PHASE; MILANKOVITCH; OCEANOGRAPHIC CIRCULATION; RELEVANT FEEDBACK; SEALEVEL CHANGE; SEDIMENT STARVATION; SEDIMENT SUPPLY; SEQUENCE STRATIGRAPHY; SHORE SEDIMENTS; SLOPE UNIT; STABLE ISOTOPES; SWITCHING SUPPLIES;

ISOTOPES; SEA LEVEL; SEDIMENTOLOGY; SEDIMENTS; TECTONICS;

STRATIGRAPHY;

BENTHIC FORAMINIFERA; CHRONOSTRATIGRAPHY; CONTINENTAL SHELF; DELTA; DEPOSITIONAL SEQUENCE; GEOLOGICAL RECORD; GLACIAL-INTERGLACIAL CYCLE; LONGSHORE TRANSPORT; MARINE SEDIMENT; OCEANIC CIRCULATION; PLANKTONIC FORAMINIFERA; PROGRADATION; SEA LEVEL CHANGE; SEQUENCE STRATIGRAPHY;

ADRIATIC SEA; MEDITERRANEAN SEA;

FORAMINIFERA;

EID: 70450196761     PISSN: 00917613     EISSN: 00917613     Source Type: Journal    
DOI: 10.1130/G25730A.1     Document Type: Article

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