FN Archimer Export Format PT J TI Understanding consequences of adaptive monitoring protocols on data consistency: application to the monitoring of giant clam densities impacted by massive mortalities in Tuamotu atolls, French Polynesia BT AF GEORGET, Stephane VAN WYNSBERGE, Simon ANDREFOUET, Serge AS 1:1;2:1;3:2; FF 1:;2:;3:; C1 Univ Reunion, CNRS, Inst Rech Dev, UMR 9220,ENTROPIE, F-98713 Arue, French Polynesi, France. Univ Reunion, CNRS, Inst Rech Dev, UMR 9220,ENTROPIE, Noumea 98848, New Caledonia. C2 UNIV LA REUNION, FRANCE IRD, FRANCE IF 3.188 TC 0 UR https://archimer.ifremer.fr/doc/00516/62717/69556.pdf LA English DT Article DE ;belt-transect;ecological monitoring;fishery;line-intersect transects;mass mortality;quadrats;sampling methods;time series;Tridacna maxima AB During long-term monitoring, protocols suitable in the initial context may have to change afterward because of unforeseen events. The outcome for management can be important if the consequences of changing protocols are not understood. In Tuamotu Archipelago atolls, French Polynesia, the density of giant clams (Tridacna maxima) has been monitored for 12years, but massive mortalities and collapsing densities forced to shift from a line-intercept transects and quadrats (LIT-Q) method to a belt-transect (BT) method. We investigated with a simulation approach the conditions (density, size structure, aggregation of giant clam populations) under which the two methods provided different results. A statistical model relating the BT density to the LIT-Q density was validated using new field data acquired on the same sites with both protocols, on two atolls. The BT method usually provided higher estimates of density than the LIT-Q method, but the opposite was found for very high densities. The shape of the relationship between measurements depended on population size structure and on aggregation. Revisiting with the model the historical LIT-Q densities suggested that densities have been underestimated in the past but previously detected trends in population trajectories remained valid. The implication of these findings for management are discussed. PY 2019 PD JUN SO Ices Journal Of Marine Science SN 1054-3139 PU Oxford Univ Press VL 76 IS 4 UT 000484404900026 BP 1062 EP 1071 DI 10.1093/icesjms/fsy189 ID 62717 ER EF